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Solar System Ambassadors/JPL/NASA

August 21, 2001

Keith Henry
Langley Research Center, Hampton, VA

RELEASE: 01-172

NASA TECHNOLOGY HELPS WEEKEND PHOTOGRAPHERS LOOK LIKE PROS

If a picture is worth a thousand words, new image-enhancement
technology jointly developed by NASA and industry will increase the
average photographer's vocabulary many times over.

This new development will especially help weekend photographers,
who use the increasingly popular digital format. Digital images of
family, friends or one's favorite hobby can be corrected for many
common problems with help from this award-winning technology.

The technology, called Retinex Imaging Processing, could be used to
enhance the billions of images captured each year by a growing
number low cost digital color cameras, color printers, and desktop
and internet publishing programs.

The process was originally developed for remote sensing of the
Earth by researchers at NASA's Langley Research Center and Science
and Technology Corp. (STC), both in Hampton, VA.

TruView Imaging Company, an affiliate of STC, has licensed the
technology from NASA and plans to market it in the form of a
software product for home, professional and industrial use by the
end of the year.

With it, amateur photographers, armed with nothing more than their
personal computers and a desire to get the most from the images
they capture, will have the ability to increase the brightness,
scene contrast, detail and overall sharpness of images with much
more ease than they can today.

What distinguishes this technology from existing image-enhancement
technologies is that it makes corrections automatically, yet allows
the end-user to manipulate the image as desired. As a result, the
average photographer is more likely to use the technology and use
it successfully.

It won't correct every image, but was impressive enough to win a
NASA Space Act Award as one of the space agency's top inventions of
the year for 1999.

"What makes Retinex technology so valuable is that every image can
stand a little improving, especially dark, low-contrast images,"
said Glenn Woodell of NASA Langley, one of three inventors of the
technology.

Dan Jobson, also of Langley and the technology's principal
investigator, teamed with co-inventors Woodell and Zia-ur Rahman of
STC to modify the technology for commercial applications.

"STC thinks consumers will find this technology so easy and
gratifying to use that people who would never consider doing
anything more than snapping a picture will let Retinex finish the
job," said Rahman.

The realistic beauty and visual impact of photographs can be
diminished, damaged or ruined by a variety of possible problems.
For example, colors and details can be lost or suppressed in
shadows or other low light level zones in a picture. These same
scenes, when viewed directly by the human observer, are vivid by
comparison to the recorded image. Consequently, the user loses both
the visual quality and emotional intensity of that captured memory.

"Existing image enhancement methods used to correct these
limitations are either insufficiently powerful or require tedious
and extensive manual user interactions," said Marisol Garcia,
Langley's Retinex commercialization project manager.

The technology is currently being refined for video image
enhancement, where the technology's high-speed, automatic
correcting features should make quick work of an otherwise tedious
and extensive process.

For publication-quality still images, visit the World Wide Web at:

http://dragon.larc.nasa.gov/retinex/pao/news

NASA GIVES POLE-TO-POLE VIEW OF CLOUD HEIGHTS AND WINDS

Scientists for the first time ever can simultaneously measure the height and
motion of clouds over Earth from pole to pole, which may improve weather forecasts.

Never before have researchers directly measured cloud heights from a single
satellite, simultaneously measured cloud heights and winds, and done this above Earth's
polar regions as well as lower latitudes.

Professor Roger Davies and graduate research assistant Akos Horvath of the
University of Arizona, Tucson, report first results on cloud winds and heights from
NASA's polar-orbiting Terra satellite's Multi-angle Imaging SpectroRadiometer in the
Aug. 1 issue of Geophysical Research Letters.

Simultaneous measurement of cloud heights accurate to within 400 meters (about
1,300 feet) and cloud winds accurate to within 3 meters (about 10 feet) per second
anywhere over the globe is a potential boon for meteorology, Davies said. While Terra is
a research satellite, not an operational satellite, the success of the radiometer's fully
automated multi-angle imaging technique "pioneers the possibility of deploying an
operational satellite to gain wind information within the atmosphere, especially over the
data-sparse areas of the oceans, for improved weather forecasts," he said.

Davies directs the Radiation, Clouds and Climate Laboratory in the University of
Arizona's atmospheric sciences department. He is co-investigator on the science team that
designed and operates the Multi-angle Imaging SpectroRadiometer.

Horvath, who is working on his doctorate in atmospheric sciences, completed his
master's degree on the feasibility of using the Multi-angle Imaging SpectroRadiometer to
measure cloud-motion wind. He will brief the National Oceanic and Atmospheric
Administration this week on the innovative cloud-tracking technique. "The wind-retrieval
technique definitely worked better than expected," Horvath said. Originally, the
researchers had intended to use wind calculations as just a step in getting accurate cloud-
top height measurements, he added.

Until Terra was launched in December 1999, cloud-motion winds were routinely
observed by only geostationary satellites. These orbit above the equator and get their
highest resolution images of the area directly below. As a consequence, satellite
information on cloud-motion winds has been more accurate nearer the equator than the
poles.

Because geostationary satellites measure reflected sunlight in only a single
direction, more than one satellite is needed to measure cloud height, or else researchers
must estimate cloud heights using assumed atmospheric temperatures or other indirect
methods, Davies said.

The Multi-angle Imaging SpectroRadiometer is a totally new instrument that
produces multi-angle imagery, one application of which is a stereoscopic view of clouds.
An array of nine cameras measures reflected sunlight in four colors from nine different
directions, covering an orbital swath 380-kilometers (about 230-miles) wide. It takes
seven minutes for a given target to be observed at all nine angles. Coupled with the multi-
angle views, this time lapse allows a fast mathematical formula to match solar reflectivity
patterns from three view angles, then unscramble the measurements to get cloud height
and motion. The data processing methodology was developed through a collaborative
effort involving researchers from the University of Arizona; NASA's Jet Propulsion
Laboratory, Pasadena, Calif.; and University College, London.

Multi-angle Imaging SpectroRadiometer data on winds may not be very useful to
operational forecasting because the instrument covers such a narrow swath of Earth,
Davies and Horvath said. Consequently, the instrument takes nine days to cover the entire
globe. A future operational satellite could feature a wide field-of-view instrument. Or,
several small satellites, each carrying three cameras operating in a single color channel,
could also be cost-effective, they said.

The Multi-angle Imaging SpectroRadiometer's principal investigator, Dr. David J.
Diner, of JPL, proposed the novel instrument for the global monitoring of clouds,
aerosols and the surface. "This instrument represents a new way of looking at Earth, and
it's exciting to see the data opening up new pathways for geophysical observation and
research," he said. Davies recognized that three of the radiometer's camera angles could
be used simultaneously to measure both cloud motion winds and cloud heights. With
help from the instrument's data processing team, Horvath analyzed the first data that
proved this concept works.

Davies and Horvath are using the Multi-angle Imaging SpectroRadiometer to
measure how much solar radiation clouds reflect from Earth, which is one of the greatest
uncertainties in understanding global climate change. The data are needed to learn how
clouds and atmospheric particles affect regional and global climate. Climatologists also
want accurate measurements of cloud height, for example, Davies said, because changing
cloud height could signal changing climate.

More information about the Multi-angle Imaging SpectroRadiometer is available
at:
http://www-misr.jpl.nasa.gov/ .

Terra is the first of a new generation in NASA Earth Observing System satellites,
part of NASA's Earth Science Enterprise. JPL is managed for NASA by the California
Institute of Technology in Pasadena.

MARS ODYSSEY MISSION STATUS

NASA's 2001 Mars Odyssey spacecraft, now 18.5 million
kilometers (11.5 million miles) from Mars on its way to a
rendezvous with the red planet on Oct. 23, remains in overall
good health. Flight controllers have turned off the Martian
radiation environment experiment after the instrument did not
respond during a downlink session last week.

Following unsuccessful attempts to reset the radiation
instrument, the mission manager and project officials have
decided to form a team to further study the anomaly over the
next several weeks and propose a course of action to recover
the instrument following Mars orbit insertion on Oct. 23.

Managers suggested that the most important thing now is
for the team members to devote their attention to achieving a
successful Mars orbit insertion, a demanding maneuver that
will require a focused team effort over the next few months.

"We have limited information on the nature of the problem
with the radiation experiment. The investigative team will
develop a fault tree containing a list of potential causes for
the behavior," said David A. Spencer, Odyssey's mission
manager at NASA's Jet Propulsion Laboratory, Pasadena, Calif.

The spacecraft's other science payloads are working as
expected. The thermal emission imaging system is made up of
an infrared imager and a visible camera, and the gamma ray
spectrometer instrument package contains a gamma ray sensor,
neutron spectrometer and high-energy neutron detector.

On Friday, Aug. 17, the team opened and closed the
valves in the spacecraft's main engine to verify that it is
working properly prior to Mars arrival. On Oct. 23, the main
engine will burn for 24 minutes so the spacecraft will be
captured into orbit around the planet.

Today, Odyssey is traveling at 24 kilometers per second
(54,600 miles per hour) relative to the Sun.

The 2001 Mars Odyssey mission is managed by JPL for
NASA's Office of Space Science, Washington, D.C. JPL is a
division of the California Institute of Technology in
Pasadena. The Odyssey spacecraft was built by Lockheed Martin
Astronautics, Denver. NASA's Johnson Space Center, Houston,
built and manages the Martian radiation environment
experiment. The thermal emission imaging system is managed by
Arizona State University, Tempe, and the gamma ray
spectrometer is managed by the University of Arizona, Tucson.

Astronaut Eileen Collins to Speak at Mars Society Convention

Air Force Colonel Eileen Collins, the first woman to command a Space
Shuttle mission and recently announced as the commander of STS-114
will speak Saturday, August 25th at the Mars Society Convention at
Stanford University.

Collins has flown on three Space Shuttle missions, including
commanding the 1999 mission to deploy the Chandra X-Ray Observatory.
She was also the first woman pilot of the initial Shuttle mission to
Mir in 1995. Collins has a BA in math and economics from Syracuse, a
masters in operations research from Stanford, and a masters in space
systems management from Webster University. She became a NASA
astronaut in 1991 and has logged over 537 hours in space. Her many
hobbies include running, golf, camping, reading, photography and
astronomy. As well as being a new member of the Mars Society, she
belongs to the U.S. Space Foundation, the AIAA, the Air Force
Association, Order of Daedalians, Women Military Aviators, and the
Ninety-Nines. She has earned many special honors and has logged over
5,000 hours in 30 different types of aircraft.

Convention Registration Still Open

This year's event offers something for every interest. For those who
have been closely following the FMARS field season at Devon Island,
we will have a full report from team members, a new video offering
from Sam Burbank, and a full track devoted to reporting the results
of the research.

U.S. Space Camp offers a discovery day for students which promises to
be loads of fun. Science fiction fans will especially enjoy the
author's panel on Friday night. Other highlights include updates and
discussion on the possibility of life on Mars, a vital dialogue on
the environmental engineering of a sustainable ecosystem, reports
from many of our partners in space advocacy, including the Planetary
Society, the International Space University and Yuri's Night and much
more.

You can register from the following link.

https://commerce.maplesquare.com/marssociety/conventionregistration.as
p

See you there.

Robert Zubrin, President
The Mars Society
On to Mars!

August 20, 2001

This Week on Galileo
August 20 - 26, 2001

Another very quiet week of cruise activities is in store for the Galileo
spacecraft. On Thursday, a test of the on-board gyroscopes is conducted.
The electronic circuits governing these gyros have shown sensitivity to the
intense radiation experienced as we fly close to Jupiter. Periodically
running these tests allows us to determine if the software scale factors
that are applied to the gyro measurements need to be updated to correctly
interpret the information. The last such test was performed on August 7,
just after the flyby, and this test will show to what extent the circuits
have recovered from the radiation effects in the intervening two weeks.

Continued playback of the data stored on the tape recorder during the Io
flyby occupies the Galileo science community this week. Data from the Solid
State Imaging camera, the Near Infrared Mapping Spectrometer, and the
instruments that measure the electromagnetic fields and particles of the
Jupiter environment are on tap. This week's playback should include the
measurements taken just as Galileo reached its closest approach to Io, at a
distance of 200 kilometers (124 miles), including views of the Isum,
Tvashtar, and Prometheus volcanoes.

For more information on the Galileo spacecraft and its mission to Jupiter,
please visit the Galileo home page at one of the following URL's:

http://galileo.jpl.nasa.gov
http://www.jpl.nasa.gov/galileo


NASA SATELLITE, UNIVERSITY OF MARYLAND AND U.S. FOREST SERVICE
PROVIDE RAPID RESPONSE TO WILDFIRES

U.S. firefighters and land managers are using the most modern
NASA satellite data to combat wildfires. NASA's Terra satellite is
providing a view of fires across the entire United States, helping
local officials manage fires more effectively, both during and
after wildfires. The effort is a collaboration between NASA, the
University of Maryland, College Park, and the U.S. Department of
Agriculture's Forest Service.

The Terra satellite beams daily images of western U.S. wildfires to
NASA within a few hours of the time that it passes over the region.
These images and active fire detections are transmitted to the
Forest Service. The images will become a regular part of the Forest
Service's fire monitoring toolkit.

Maps derived from the data show daily active fires and areas that
were burned during previous days. In the future, other Terra-
derived data will help teams of scientists rehabilitate burned
areas. They will use burn severity maps -- derived from satellite
and ground measurements -- to prevent further erosion, soil loss
and adverse impacts to water quality. Terra data will provide a
quick look, which can then be refined on the ground. The maps will
also help scientists identify critical wildlife habitat affected by
the fire and facilitate reforesting an area.

"NASA remains deeply committed to working cooperatively with its
sister agencies to monitor and combat wildfires across the nation,"
said Ghassem Asrar, NASA's Associate

Administrator for the Office of Earth Science. "Our investment in
the Terra Earth Observing System is starting to pay tremendous
dividends to the American taxpayer."

To use the Terra data to tackle forest fires, the three
institutions are integrated under the Rapid Response Project, which
includes a complex communications network. Rob Sohlberg at the
University of Maryland's Department of Geography leads the project
with Jacques Descloitres at NASA's Goddard Space Flight Center.
This program was created in response to the 2000 fire season, with
its extensive wildfires in Idaho and Montana.

"The Active Fire Maps offer the potential for understanding the
'big picture' when working on resource allocations decisions," said
Alice Forbes, Deputy Director for Forest Service Fire and Aviation
Operations at the National Interagency Fire Center, Boise, ID. "The
maps can also help the public understand where the fires are
located, and give them a look at the burned areas after fire
season."

By October, the Forest Service will have the capability to produce
its own fire images within minutes of a Terra overpass. The Forest
Service is currently building a processing center, called the
Remote Sensing Applications Center (RSAC), in Salt Lake City, UT,
to generate real-time images of western wildfires. However, the
Forest Service will still receive imagery of the eastern United
States from the University of Maryland and NASA.

The University of Maryland and NASA have developed all of the
needed software, which will be installed at the USFS direct
broadcast station. The Forest Service has developed the
corresponding software that creates the maps from the Terra data
using standard Forest Service mapping techniques.

"The University of Maryland sends images and active fire location
information daily to RSAC staff who are overlaying state boundaries
and topographical features on the images to best determine where
fires are occurring," said Keith Lannom, the Operations Program
Leader at RSAC. These maps show current active fire areas in real-
time on the Internet."

Data for tracking fires comes from Terra's Moderate Resolution
Imaging Spectroradiometer (MODIS). The Terra spacecraft is part of
NASA's Earth Science Enterprise, a long-term research effort being
conducted to determine how human-induced and natural changes affect
our global environment.

Wei Min Hao, the Project Leader of the Fire Chemistry Project at
the Forest Service's Fire Science Laboratory in Montana is
developing a method to track smoke dispersed by wildfires, and to
determine the impact that it has on regional air quality. Hao said,
"During fires where there are large amounts of smoke,
reconnaissance planes that normally map fires can't fly into an
area, but MODIS can provide those pictures from space." Dr. Yoram
Kaufman from NASA is working with Dr. Hao on these products.

The MODIS Rapid Response Fire Maps can be accessed through the
National Interagency Fire Center Web site (click on RSAC Fire Maps
link) at:

http://www.nifc.gov/firemaps.html

For additional information, please see:

http://www.gsfc.nasa.gov/topstory/20010810modisfiremonitor.html.


NASA COMPUTER TOOL SMOOTHS FLOW OF AIR TRAFFIC

Air traffic controllers will be able to make decisions about air traffic with greater accuracy thanks to a new NASA software tool.

Researchers at NASA's Ames Research Center, located in California's Silicon Valley, recently monitored more than 1,000 take-offs, landings and overhead flights near Denver to test the en-route data exchange (EDX) tool. The tool allows for the "real-time" delivery of flight data to automated air traffic management software, giving controllers the ability to predict aircraft position and avoid potential conflicts.

"The ability to accurately predict aircraft trajectories more than 20 minutes in advance is crucial to the success of air traffic management," according to Rich Coppenbarger, EDX technical lead. "EDX allows automation used for air traffic control decisions to be more accurate, thereby increasing fuel efficiency and system capacity, and reducing controller workload," he added.

EDX delivers 32 types of data from the plane to air traffic controllers, who are using NASA's Center-TRACON (Terminal Radar Approach Control) Automation System, or CTAS. Some data, including aircraft speed, weight, flight plans and weather conditions, are processed immediately, and the rest are stored for later analysis.

"Field experience has shown that controllers must have confidence in the accuracy of underlying trajectory predictions in order to utilize our automation effectively. EDX provides that level of trust by providing a wealth of accurate and timely data," said Coppenbarger.

With cooperation from United Airlines, 48 Boeing 777 aircraft received EDX software upgrades. The 777 was chosen because of its state-of-the-art avionics and advanced handing of 'datalink' information.

The six-month test of EDX was conducted at the Denver Air-Route Traffic Control Center with the assistance of the Federal Aviation Administration (FAA), Washington, D.C.; Honeywell, Morristown, NJ; and United Airlines, Chicago.

The next step is evaluation of the tool's capabilities for future application to real-time flight plan development and modification. This capability can be viewed as an important step toward attaining Free Flight, which is a FAA program that will give pilots the freedom to choose their own flight paths in real time.

The tools within the CTAS suite are designed to help air traffic controllers manage the increasingly complex air traffic flows at large airports and en route. The tools in CTAS benefit air travelers by reducing delays while maintaining safety.

EDX is being developed under the Advanced Air Transportation Technologies (AATT) project, a part of NASA's Aviation Systems Capacity Program led by Ames Research Center. Ames has been conducting air traffic control research and development since the mid-1980s.


CONTRACT RELEASENASA EXERCISES DELTA II CONTRACT OPTION FOR ESSP 3/CLOUDSAT

NASA today announced that it is exercising a contract option
with the Boeing Co., Huntington Beach, CA, for a Delta II vehicle to
launch the ESSP 3/CloudSat mission. The spacecraft are planned for
launch on April 30, 2004.

This firm-fixed price option is covered under the NASA Med-Lite
contract awarded to Boeing in 1996. NASA's total launch services
budget for the ESSP 3/CloudSat mission is valued at approximately
$60 million.

ESSP-3 (formerly Picasso-CENA), the third mission of the NASA Earth
System Science Pathfinder (ESSP) program, will carry three
instruments to study clouds and chemicals in the Earth's atmosphere.
The ESSP-3 satellite flies in formation with the Aqua spacecraft to
provide a comprehensive global dataset which will greatly improve our
ability to predict future climate change.

ESSP-3 is a collaboration between NASA's Langley Research Center
(LaRC), Hampton, VA; the French space agency CNES, Paris; Hampton
University, Hampton, VA; the Institut Pierre Simon Laplace (IPSL),
Paris; and Ball Aerospace Corp., Boulder, CO.

CloudSat's trio of satellites will be the first spacecraft to study
clouds on a global basis, contributing to better predictions of
clouds and their role in climate change. The CloudSat mission is a
partnership between Colorado State University, Fort Collins, CO;
NASA; the Jet Propulsion Laboratory, Pasadena, CA; the Canadian Space
Agency, Saint-Hubert; the U.S. Air Force; the U.S. Department of
Energy; and Ball Aerospace & Technologies Corp., Boulder, CO.

NASA's ESSP 3/CloudSat Program is managed by the Earth Science
Enterprise and NASA's Earth System Science Pathfinder Program at NASA
Headquarters, Washington, D.C., and by the Jet Propulsion Laboratory.


MAHONE NAMED ACTING ASSOCIATE ADMINISTRATOR FOR PUBLIC AFFAIRS

Administrator Daniel S. Goldin today named Glenn Mahone, NASA
Press Secretary and Senior Advisor, as the new Acting Associate
Administrator for Public Affairs.

Mahone was first appointed to the Administrator's office in April
2000. As a senior advisor and press secretary, he provided advance
and on-site communications guidance, coordinating the
Administrator's appearances for national and local events, often
involving the White House, members of Congress and aerospace
industry leaders.

"I am delighted Glenn has agreed to accept this important
appointment," said Administrator Goldin. "His guidance and advice
are deeply respected by NASA's senior managers and his new
leadership role will be vital to the continued success of our
public affairs outreach efforts."

Before joining NASA, Mahone served as a key advisor to the U.S.
Equal Employment Opportunity Commission, providing advice on
communications strategy and directing the preparation of speeches
and other support material for internal and external use. In 1997,
he was a commercial sales and marketing manager for ADT Security
Services, Baltimore, MD.

Mahone's previous experience also includes work as management
consultant to the President and CEO of Stephens Engineering
Company, Inc., Lanham, MD, and he was a consultant for employment
and training for the U.S. Department of Labor, Washington, DC.

Before coming to Washington, Mahone was Director of Information
Services and Press Secretary for the Arkansas Secretary of State
and he worked as Director of Public Affairs for KHTV-TV, a CBS
television network affiliate in Little Rock.

Mahone has a Bachelor of Science Degree in Communications from the
University of Central Arkansas, with a minor in journalism.


ADMINISTRATOR NAMES DIRECTOR OF SECURITY MANAGEMENT & SAFEGUARDS

Administrator Daniel S. Goldin today announced the appointment
of David Saleeba as Director of the newly formed Office of Security
Management and Safeguards at NASA Headquarters, Washington, DC.

His principal responsibilities include the oversight and assessment
of the agency's physical and information/technology security
programs, as well as representing NASA to the external security
community, and advising the Administrator on all security issues.

"Safety and security are priority issues for NASA," said
Administrator Goldin. "Saleeba's extensive experience will be an
important asset to this agency and I am pleased he has decided to
accept this opportunity."

Saleeba brings to NASA nearly 30 years experience in law
enforcement and security, including 26 years with the U.S. Secret
Service, most recently as Special Agent in Charge and Chief of the
Secret Service's Headquarters Intelligence Division, Washington,
DC.

Past assignments with the Secret Service included tours in Miami,
New York, two White House protective assignments, and five years as
the Special Agent In Charge of the New Mexico District.

Saleeba has also led liaison and cooperative projects with local,
state, and federal law enforcement, three Air Force bases, and the
Los Alamos and Sandia National Research Laboratories.

His experience includes security operations in all 50 states, 59
foreign countries, and he has testified before Congress on
legislative initiatives affecting federal law enforcement and
counterintelligence.

In the early 1970's, he served on the Metro-Dade County Police
Department in Miami, FL, as police officer and detective with the
department's Organized Crime Bureau.

Saleeba is a 1971 graduate of Pennsylvania State University and
currently lives with his wife, Kathy, in Virginia.


August 18, 2001

Cassini Weekly Significant Events
for 08/09/01 - 08/15/01

The most recent spacecraft telemetry was acquired from the Madrid
tracking station on Tuesday, August 14. The Cassini spacecraft is in an excellent
state of health and is operating normally. Information on the spacecraft's
position and speed can be viewed on the Present Position web page
("
http://www.jpl.nasa.gov/cassini/english/where/").

Recent spacecraft activities include a Magnetospheric and Plasma Science

observation, two Radio and Plasma Wave Science (RPWS) High Frequency
Receiver Calibrations, and an RPWS Instrument Expanded Block Test. Real-time
commands were uplinked to the spacecraft as planned to update the definition of
the X-Band and Ka-Band body vectors, to perform routine Command & Data
Subsystem (CDS) memory readouts of the sequence registration table and
non-interfering error logs, and to clear the AACS High Water Marks.

In support of Tour planning, a program was uplinked that will
characterize the behavior of the X-Band Traveling Wave Tube Amplifier when operated in
the manner planned to be used during the tour. This program will execute later this
week.

Mission Planning continued timeline development for tour Orbit Trim
Maneuvers (OTMs). It was determined that nominal OTMs can be placed in the middle
ofnearly all expected DSN passes without encountering background sequence
telemetry mode changes, which could interfere with storage of OTM data
and subsequent science playback.

The Cassini Information Management System 1.3 was delivered. This
delivery provides Extensible Markup Language (XML) export capability to support
near-term Science Operations Plan development milestones.

The full Integration Test Laboratory retest of all modules for Mission
Sequence Subsystem D7.6 completed successfully.

Mission Support & Services Office Security personnel have begun leading
the annual Cassini security training courses, in an effort to make sure all
Cassini team members are informed of the up-to-date security policies and
procedures.

Cassini Outreach personnel made a presentation on Saturn and Cassini to
30 college and high school educators at a course jointly sponsored by JPL
and California State University, Northridge. Thirty-three Solar System
Educators were updated on Cassini results from Jupiter and practiced using an
activity from the Saturn Educator Guide. These master teachers will share their
expertise with other teachers in their communities and elsewhere, so
that more solar system exploration materials will be used in classrooms
through out the U.S.


NASA PROGRAM BRINGS THE STARS HOME

Teachers are learning how to take control of a telescope located high above Los Angeles.
They will learn how to operate the telescope using the Internet and how to download bountiful
images of far out galaxies right to their classroom computers.

The Telescopes In Education program, managed by NASA's Jet Propulsion Laboratory,
Pasadena, Calif., is sponsoring the two-day workshop on Aug. 17 and 18 for more than 15
teachers. The program aims to give educators and students access to research-quality telescopes
and charge-coupled device cameras created at JPL and located at the Mount Wilson Observatory.

"We realize many people live in remote areas and that visits to observatories by schools
are sometimes not feasible," said Gilbert Clark, program manger. "We wanted to bring science
and astronomy home. That means giving teachers the access and the ability to remotely operate
a telescope from the comforts of their classroom."

Educators and students can reserve observation time lasting from one hour to all night for
any evening of the week. Special observation times or long-term, repetitive observing runs require
special arrangement. More information about the program is available online at
http://tie.jpl.nasa.gov/ .

In the 1999-2000 school year, the program enabled more than 10,850 students nationwide
from kindergarten through high school, to conduct astronomical observations and meaningful
research. Over the last nine years, the Telescopes In Education program has created a legacy of
students who have learned science through this program of hands-on astronomy.

Telescopes In Education is a NASA education outreach program sponsored by NASA's
High Performance Computing and Communications Learning Technologies Program, the Office
of Space Science and the Office of Human Resources and Education. JPL space exploration
missions, businesses and numerous volunteers also support the program. Managed for NASA by
the California Institute of Technology, JPL is the lead U.S. center for robotic exploration of the
solar system.


GRAND CANYON TOUR, NASA STYLE

If schedule or budget kept you from visiting the Grand Canyon this summer, you
can still enjoy the stunning features created by the Colorado River over the centuries,
courtesy of NASA.

A new image shows a simulated true-color perspective view of the Arizona
natural wonder. Facing north-northeast, the view is dominated by the North Rim, and it is
about 30 kilometers (19 miles) wide at the horizon. Grand Canyon Village is on the lower
right of the image, and the Bright Angel Trail is visible as it crosses the Tonto Plateau.
The trail also goes to Phantom Ranch, the green area across the Colorado River.

The image was taken by the Advanced Spaceborne Thermal Emission and
Reflection Radiometer, an imaging instrument flying on NASA's Terra satellite.

The image is available at:

http://www.jpl.nasa.gov/images/earth/usa/west.html .

More information on the mission is available at:

http://asterweb.jpl.nasa.gov .

The Terra spacecraft, the flagship of a fleet of satellites dedicated to
understanding our global environment, is part of NASA's Earth Sciences Enterprise, a
long-term research program dedicated to understanding how human-induced and natural
changes affect our world.


August 17, 2001

NOAA Honors Students with the Dr. Nancy Foster Scholarship Award

The Department of Commerce's National Oceanic and Atmospheric
Administration (NOAA), awards the newly established Dr. Nancy Foster
Scholarship to five outstanding graduate-level researchers, in the fields
of oceanography, marine biology and maritime archaeology.
Soon after the death of NOAA's Dr. Foster, in June of 2000, Congress
created the scholarship as a means of honoring her life's work and
contribution to the nation. The funding is drawn from the National Marine
Sanctuaries Act which is administered by the NOAA's National Ocean Service
(NOS). The current funding enables NOAA to award five scholarships. Each
scholarship recipient will receive an annual stipend of $16,800 and up to
$12,000 annually for tuition. Doctorate students are eligible to continue
the scholarship program for four years and Masters-level students for two
years.

This is the first year of the program and NOAA received over 500
applications for the five awards. "We received a large number of
applications from a pool of extremely well-qualified students. It is great
to see such interest in the first year of the program," said NOAA Acting
Administrator, Scott Gudes. Students were evaluated based on financial
need, academic excellence, recommendations and a statement of intent which
also indicated the student's research and career goals.

The five recipients are as follows:

Winnie Wing Yee Lau, Seattle, Washington: Ms. Wing Yee Lau is currently
pursuing a doctorate in biological oceanography at the University of
Washington. As an undergraduate, Ms. Wing Yee Lau majored in both
integrative biology and environmental sciences at the University of
California at Berkeley. Ms. Wing Yee Lau decided to pursue a graduate
degree in basic scientific research not only because she loved making new
discoveries but also because she realized that a solid scientific knowledge
is the foundation of effective management of ecosystems.

Ku'ulei S. Rodgers, Waimanalo, HI: Ms. Rodgers is from and is currently
pursuing a doctorate in marine biology. Ms. Rodgers was born and raised on
the island of O'ahu, the main island in the Hawaiian chain. Ms. Rodgers
has always been employed in the marine field. She spent several years
working as an ocean recreation specialist teaching drownproofing to public
school children and as a marine mammal trainer at an oceanarium. However,
Ms. Rodgers' career in marine biology began late in life at Windward
Community College where she quickly developed a strong background in marine
science. Rodgers continued her education by earning her master's degree at
the University of Hawai'i at Manoa where she narrowed her focus to coral
reef research. Rodgers' current doctoral work also focuses on coral reef
research. Rodgers is specifically working to identify bioindicators that
may serve as an early warning of coral reef decline.

Stefan Claesson, Biddeford, Maine: Mr. Claesson is pursuing his doctorate
in natural resources at the Universrity of New Hampshire. Mr. Claesson
received his bachelor's degree from Boston University and his masters in
nautical archeology from Texas A&M University. Born in Worcester,
Massachusetts to Swedish immigrants, and raised in Cape Neddick, Maine, he
has always had a strong connection to the sea and an equally strong
interest in maritime history and archaeology. Mr. Claesson has conducted
archaeological surveys for shipwrecks and other vestiges of maritime
culture along the southern coast of Maine for the past five years. Mr.
Claesson is currently working to develop a Geographic Information System
for the management and preservation of maritime cultural resources in New
England.

Jennifer Wagner Whiteis, Trumansburg, N.Y.: Ms. Whiteis is pursuing a
doctorate in oceanography. Ms. Whiteis started her academic career at the
University of North Carolina in Wilmington where she studied earth sciences
and she then transferred to Cornell University where she graduated with a
bachelors degree in geology. While studying at Cornell, Ms. Whiteis was
awarded a NASA Space Grant Fellowship to carry out a project using remote
sensing techniques to study physical ocean parameters that impact coral
disease in the Caribbean Sea. This experience motivated her to continue
studies with a more detailed, in-depth research project using a combination
of multiple satellite sensors and in situ data to examine the impact of
global climate change on Caribbean corals.

Laurie Ann Sorabella, Gloucester, VA: Ms. Sorabella is currently pursuing
a masters in marine biology at the Virginia Institute of Marine Science.
Ms. Sorabella's research centers on estuarine and coastal habitat
restoration and on citizen involvement in restoration initiatives. Ms.
Sorabella's thesis, entitled "Oyster and Seagrass Interactions in
Ecological Restoration," has two objectives. First, to define the most
desirable oyster strain for use as broodstock in oyster reef restoration
and second, to characterize water quality changes associated with a
restored oyster reef and estimate the potential for reefs to create a more
habitable environment for seagrasses. Before graduate school, Ms.
Sorabella became inspired by the power of community involvement when she
worked as Virginia Habitat Restoration Coordinator for the Chesapeake Bay
Foundation.

"Throughout her career, Dr. Foster was well respected as a personal
supporter of mentoring, a champion of diversity, and an advocate of fair
and equal treatment of all people in the workplace. This scholarship is an
excellent way to pay tribute to her life, "added Gudes.

The applications represented all the coastal regions of the United States,
including several from Alaska, Hawaii, and Puerto Rico. Applications were
ranked by a panel of NOAA employees and finalists selected based on the
ranked scores. A separate panel selected the five award winners for the
2001-2002 school year from the finalists.

A call for applications for the 2002-2003 school year is expected to be
released some time this fall.

NOAA's National Ocean Service is a federal agency devoted to exploring,
understanding, conserving, and restoring the nation's coasts and oceans.
NOS promotes safe navigation, supports coastal communities, sustains
coastal habitats and mitigates coastal hazards. NOS balances environmental
protection with economic prosperity and leads the effort to ensure that our
nation's coastal areas remain safe, healthy and productive. NOS is an
agency of the U.S. Department of Commerce's National Oceanic and
Atmospheric Administration.

For more information, check the Foster scholar Web site at
http://fosterscholars.noaa.gov


NOAA DELIVERS LIFE-SAVING DISASTER-PREPAREDNESS INFRASTRUCTURE
AND SYSTEMS TO CENTRAL AMERICA
Ceremony in Nicaragua Marks Final Phase of $16M NOAA Reconstruction Effort

Representatives from the United States and Nicaragua are marking the final
phase of NOAA's $16 million project at a ceremony in Managua, Nicaragua on
August 22. A team of weather, hydrology and ocean experts from the
Commerce Department's National Oceanic and Atmospheric Administration
(NOAA) are nearing completion of a $16 million disaster recovery program in
five Central American countries devastated in 1998 by Hurricane Mitch, the
deadliest Atlantic hurricane in more than two centuries.
"NOAA is committed to working with our international partners to safeguard
lives, property and sensitive ecological resources," said Scott B. Gudes,
acting administrator for NOAA. "This project marks a critical step to
improving weather forecasting and disaster-preparedness in Central America
and creating an international standard for information sharing and
cooperation."

The NOAA reconstruction project is part of an overall $17 million
Department of Commerce (DOC) effort to address problem areas identified as
critical to mitigating against the effects of future natural disasters in
Central America and the Caribbean. The DOC plan called for NOAA, the
National Institute for Standards and Technology (NIST) and the
International Trade Administration (ITA) to address five areas: (1) Base
infrastructure; (2) Forecast and Early Warning Systems; (3) Disaster
Preparedness and Response; (4) Sustainable, Resilient Coastal Communities;
and (5) Economic Revitalization.

NOAA's efforts focused on two key areas; early warning & preparedness, and
coastal assistance:

EARLY WARNING & PREPAREDNESS

Recognizing Central America had limited severe weather warning and
forecast services, NOAA helped create the infrastructure necessary to
improve forecasting and early storm warnings through disaster preparedness
and response. Key elements include:

$ Replaced damaged and expanded automatic meteorological and hydrological
stations.
$ Reestablished upper air station in Honduras critical for hurricane
forecasting.
$ Provided automated precipitation gauges for real-time data.
$ Improved capabilities to receive and interpret satellite imagery for the
region.
$ Established a regional, seasonal climate prediction system.
$ Provided a satellite ground station that brings high resolution digital
imagery from NOAA's Geostationary Operational Environmental Satellites (GOES).
$ In cooperation with U.S. Geological Survey (USGS) rebuilt tools to
measure water levels, tides and geodetic positioning networks.
$ NOAA and USGS provided technology for state-of-the-art river and flood
forecast systems.

Retired General Jack Kelly, NOAA's National Weather Service (NWS) director
said, "While we can't stop the catastrophic floods from hurricanes, we can
do something to help local officials warn residents. Furthermore, all
Americans will be better protected because the new data from our
international partners will improve our hurricane forecasts." Weather data
from Central America provides critical insight into where a hurricane might
go and how strong it will be.

COASTAL ASSISTANCE

NOAA also advised on regional watershed management and assisted in
building more sustainable and resilient coastal communities. NOAA's
environmental scientists are improving coastal management in the region to
lessen the impacts of future weather disasters and improve response
capabilities. This includes:
$ improved capabilities along coasts to cope with impacts of hurricanes
$ installed tide gauge networks
$ rebuilding aquaculture shrimp industry and providing more information on
water circulation and contaminant levels in the Gulf of Fonseca - an
important bay on the Pacific coast.

"A degraded environment threatens local economic prosperity and the well
being of coastal residents," said Margaret Davidson, acting director of the
National Ocean Service (NOS). "The coastal area of the Gulf of Fonseca is a
vital economic resource to the region. Its estuaries help support the
community and small-scale commercial fishing, shrimp aquaculture and salt
production. We are providing information to improve coastal management and
maintain economic vitality."

NOAA's reconstruction projects are expected to be completed by December
2001 and is part of a $621 million hurricane reconstruction project funded
by the U.S. Agency for International Development (USAID).

The Commerce Department's National Oceanic and Atmospheric Administration
(NOAA) is dedicated to enhancing economic security and national safety
through the prediction and research of weather and climate-related events
and providing environmental stewardship of our nation's coastal and marine
resources. To learn more about NOAA, please visit http://www.noaa.gov

To learn more about Hurricane Mitch and NOAA's reconstruction program,
please visit: Hurricane Mitch Report -
http://www.nhc.noaa.gov/1998mitch.html
Hurricane Mitch satellite images -
http://www.ncdc.noaa.gov/ol/reports/mitch/mitch.html
NOAA GOES Homepage -
http://www.oso.noaa.gov/goes



CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109
http://www.jpl.nasa.gov

Guy Webster

Galileo Millenium Mission Status
August 16, 2001

NASA's Galileo spacecraft is transmitting to Earth scientific information
from its dash past Jupiter's moon Io last week, including top-priority
measurements of magnetic forces above Io's north pole.

A first look at the data already suggests that Io's internally generated
magnetic field is either absent or quite weak, said the principal
investigator for Galileo's magnetometer instrument, Dr. Margaret Kivelson of
the University of California, Los Angeles. Stronger conclusions will have to
await more analysis. Determining whether Io has an intrinsic magnetic field
is the primary science goal for the flyby on Aug. 6, Universal Time, and for
Galileo's next encounter, an Oct. 16 pass near Io's south pole.

Sampling of other early data indicates that Galileo's camera appears to have
resumed functioning in time to capture some of the final images planned
during last week's flyby, said Dr. Eilene Theilig, Galileo project manager
at NASA's Jet Propulsion Laboratory, Pasadena, Calif. Some exposures planned
while Galileo was closest to Io were lost because of an intermittent
electronic problem that has affected the camera for more than a year.
Project engineers believe the problem probably results from cumulative
exposure to intense natural radiation near Jupiter.

"We're now expecting to get images from five of the 16 planned observations,
including global images of Io," Theilig said. Stored data on Galileo's tape
recorder from the camera and other instruments will continue to arrive at
Earth antennas of the JPL-managed Deep Space Network throughout the next
eight weeks.

Galileo has been orbiting Jupiter since 1995. After its original two-year
tour of the Jovian system, NASA extended the intrepid robot's mission three
times to take advantage of Galileo's continuing ability to return valuable
scientific information. The spacecraft has handled more than three times as
much radiation from Jupiter's radiation belts as it was engineered to
withstand. Its nuclear electrical power source continues to provide reliable
electricity for its on-board instruments, computers, radio and other
systems.

Data from the Aug. 6 flyby are still being analyzed to determine whether
Galileo flew through an active plume as it skimmed over Io. The Tvashtar
volcanic area near Io's north pole was spouting a tall plume when last
observed seven months earlier. Io is the most volcanic world known.
Observations by Galileo's infrared and radiometer instruments, as well as
the camera's images, should provide new details about volcanic activity near
the pole, Theilig said.

Determining whether Io has an intrinsic magnetic field will narrow the
possible models for the moon's interior and give better understanding of
planetary interiors in general, said Galileo Project Scientist Dr. Torrence
Johnson of JPL. Magnetic fields such as those that exist at Earth, Jupiter
and Jupiter's moon Ganymede are generated by movement of fluid material deep
inside.

Io's density and heat output tell scientists that it, like Earth, has a
molten iron core. If Io indeed lacks an intrinsic magnetic field, that would
suggest its molten core lacks the vigorous convective motion that is
believed to result in Earth's field, Johnson said. "That might fit a model
where Io's core is swaddled by a hot, warm blanket that heats the core from
outside," he said.

Fluctuations in the pull of Jupiter's gravity as the moon's distance from
the planet varies are believed to generate much of Io's internal heat by
flexing a stiffer mantle layer surrounding Io's core. New magnetic data will
help scientists evaluate and refine that model of Io's heating, Johnson
said.

Data from instruments that monitor particles and energy fields around the
spacecraft will also help in understanding currents that couple Io to the
atmosphere and ionosphere of Jupiter, he said.

Additional information about Galileo, Io and Jupiter is available online at
http://galileo.jpl.nasa.gov. JPL, a division of the California Institute of
Technology in Pasadena, manages the Galileo mission for NASA's Office of
Space Science, Washington, D.C.


August 17, 2001
Kirsten Larson
Headquarters, Washington

Doug Peterson
Johnson Space Center, Houston, TX

Release: H01-167

NASA NAMES 23 ASTRONAUTS AND COSMONAUTS TO SHUTTLE FLIGHTS IN 2002

NASA has named crew members to three missions scheduled to visit the
International Space Station in the second half of 2002.

STS-112 (scheduled for July), STS-113 (August) and STS-114 (November)
will involve assembly work, and the last two also will exchange space
station expedition crews. In all, these missions will carry 23
astronauts and cosmonauts, including nine first-time flyers.

STS-112, commanded by Jeffrey S. Ashby (Capt., USN), will deliver a
segment of the space station's truss and equipment to help spacewalkers
move around the station's exterior. Pamela A. Melroy (Col. select, USAF)
will serve as pilot. Mission specialists include David A. Wolf (M.D.),
Piers J. Sellers (Ph.D.), Sandra H. Magnus (Ph.D.) and Fyodor N.
Yurchikhin, RSC Energia.

Ashby has flown twice, on STS-93 in 1999 and STS-100 this year. Melroy
flew on STS-92 in 2000. Wolf first flew in 1993 on STS-58; in 1997 he
traveled to the Russian space station Mir, where he spent 123 days.
Sellers, Magnus, and Yurchikhin will be making their first trips into
space.

STS-113, commanded by James D. Wetherbee (Capt., USN), also will carry a
truss segment, along with additional equipment to assist spacewalkers.
Pilot Christopher J. Loria (Lt. Col., USMC) will join Wetherbee on the
flight deck. Michael E. Lopez-Alegria (Capt. select, USN) and John B.
Herrington (Cmdr., USN) will serve as mission specialists.

Wetherbee, a veteran astronaut, has been in space five times: STS-32 in
1990, STS-52 in 1992, STS-63 in 1995, STS-86 in 1997 and STS-102 in
2001. Loria and Herrington are first-time flyers, and Lopez-Alegria will
take his third trip to space, having flown on STS-73 in 1995 and STS-92
in 2000.

The Expedition Six space station crew -- Commander Kenneth D. Bowersox
(Capt., USN), Donald A. Thomas (Ph.D.) and Nikolai M. Budarin, RSC
Energia -- will travel to the station aboard STS-113. The Expedition
Five crew, made up of Valeri G. Korzun (Col., Russian Air Force), Peggy
A. Whitson (Ph.D.) and Sergei Y. Treschev, RSC Energia, will return to
Earth on STS-113.

Bowersox was a member of STS-50 in 1992, STS-61 in 1993, STS-73 in 1995
and STS-82 in 1997. Thomas previously orbited Earth during STS-65 in
1994, STS-70 in 1995, STS-83 in 1997 and STS-94 in 1997. Budarin returns
to space for his third long-duration flight after stays on Mir in 1995
and 1998. Expedition Five's Korzun takes his second long-duration trip
to space after a stay at Mir that ended in 1997, while Whitson and
Treschev will make their first trips into space.

STS-114, which had been labeled STS-113 in earlier planning schedules
and news releases, will be commanded by Eileen M. Collins (Col., USAF)
and piloted by James M. Kelly (Lt. Col., USAF). The mission is a space
station utilization and logistics flight. The mission includes Soichi
Noguchi (NASDA) and Stephen K. Robinson (Ph.D.) as mission specialists.
The mission will return Expedition Six to Earth and take Expedition
Seven to the station. Expedition Seven is comprised of Yuri I.
Malenchenko (Col., Russian Air Force), Sergei Moschenko, Khrunichev
Space Center, and Edward T. Lu (Ph.D.).

Collins served as pilot on STS-63 in 1995 and STS-84 in 1997, and
commanded the STS-93 mission in 1999. Kelly flew his first mission
aboard STS-102 earlier this year. Robinson, having flown on STS-85 in
1997 and STS-95 in 1998, also serves as a backup crewmember for
Expedition Four. Malenchenko served as commander of Mir 16 and flew on
STS-106 in 2000. Moschenko is making his first space flight, while Lu
flew aboard STS-84 in 1997 and STS-106 in 2000. Noguchi will be taking
his first flight into space.

Further information is available on the Internet:

Crew Biographies http://www.jsc.nasa.gov/Bios/

International Space Station http://spaceflight.nasa.gov

Space Shuttle Launch Schedule
http://spaceflight.nasa.gov/shuttle/future/index.html

JET PROPULSION LABORATORY

Having a Ball on Mars

An amusing accident in the Mojave desert has inspired a new kind of Mars
rover -- a two-story high beach ball that can descend to the Martian
surface, land safely, and explore vast expanses of the Red Planet.

FULL STORY at

http://science.nasa.gov/headlines/y2001/ast17aug_1.htm?list448368


CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109 TELEPHONE (818) 354-5011
http://www.jpl.nasa.gov

Contact: Colleen Sharkey
Rosemary Sullivant

NASA SCIENTISTS BECOME HURRICANE CHASERS

Scientists from NASA's Jet Propulsion Laboratory, Pasadena, Calif., will head into
hurricanes this summer, hoping to improve predictions of these deadly storms by using
new data-collecting technology.

The four scientists are part of NASA's fourth Convection and Moisture Experiment,
a massive field experiment based at Jacksonville Naval Station, Fla., from Aug.16 through
Sept. 24. Their instruments will be on two NASA aircraft as they fly over, through and
around selected hurricanes in the Caribbean, the Gulf of Mexico and the Atlantic.

The goal of the experiment is to take the mystique out of hurricanes. By examining
how a hurricane evolves and behaves, investigators hope to make possible more accurate,
longer-range forecasts. Since evacuation is often the key to saving lives during a hurricane,
researchers are paying special attention to a hurricane's behavior when it hits land.

Participants in this year's Convection and Moisture Experiment from JPL include:

--Bjorn H. Lambrigtsen, who led the team that designed and built the High Altitude
Monolithic Microwave Integrated Circuit Sounding Radiometer for this mission. An
advanced atmospheric microwave sounder, the instrument can "see" through clouds. On
previous investigations of this project, two separate microwave sounders recorded
temperature and humidity. This new instrument, smaller and lighter than its predecessors,
will have the ability to do both.

The radiometer will fly in one of the wing pods of the high-altitude Earth Research-
2 aircraft, a former U2 spy plane. From an altitude of about 20 kilometers (65,000 feet), it
will scan the atmosphere below the plane from side to side with a searchlight-type beam
and map the temperature, humidity and cloud distributions inside a hurricane.

Lambrigtsen and his team will participate in all flights of the Earth Research-2
craft. From their instrument's measurements, they will derive vertical profiles of
temperature, water vapor and liquid water. They will also estimate rain rates and create an
ice-particle scattering index, which will be used to develop a formula for calculating cloud
ice. Co-investigators are Drs. Lance Riley and Evan Fishbein, also from JPL.

-- Dr. Robert Herman, who will lead the JPL Laser Hygrometer team. The laser
hygrometer is a miniature laser spectrometer for rapid measurements of water vapor.
During this mission, the instrument will be mounted on a NASA DC-8 aircraft to measure
water vapor as the airplane flies through tropical hurricanes. The data will help scientists
understand just how much moisture the air can hold before ice clouds form. The instrument
will also provide information on latent heat, the heat released when water condenses,
which is an important energy source that drives storms. These data should provide a better
understanding of the processes that regulate water in the atmosphere and tropical storms.

-- Dr. Michael Mahoney, the principal investigator for the DC-8 Microwave
Temperature Profiler and the Earth Research-2 Microwave Temperature Profiler. The
instruments scan vertically in each aircraft's flight direction. Looking straight down,
straight ahead and straight up, they measure temperature at different frequencies to create a
complete temperature profile.

On the DC-8, the Microwave Temperature Profiler displays air temperature data in
real-time and is updated every 15 seconds. An experimenter onboard the DC-8 can control
this real-time data and provide it to scientists immediately. The temperature profile of the
atmosphere is a vital part of hurricane research because it helps scientists understand the
stability of the atmosphere. The instrument can also help pinpoint the exact location of the
troposphere, the lower part of Earth's atmosphere. In addition, it can measure the flow of
air parcels to determine if there are gravity waves in the atmosphere that could affect the
level of ozone depletion.

On the Earth Research-2 aircraft, the microwave temperature profiler operates
autonomously, and the data is processed later.

-- Dr. Eastwood Im, who will administer the Dual Frequency Airborne
Precipitation Radar, an airborne dual-frequency radar that will measure the 3-D structure
of rainfall. Two crucial parts of the new instrument -- the pressure box and antenna -- are
from a previous airborne radar developed by JPL, called Airborne Rain Mapping Radar.
The new instrument is an improvement over the earlier radar because it has two
frequencies, which will improve rainfall measurements, and can process data in real time.

The instrument team plans to fly this radar in a rotating figure-four pattern across
the rainstorm through the hurricane's eye, as well as through the rainbands at the storm's
edge. Data collected will help determine rain rate, vertical motion and location of melting
ice along the DC-8 flight track below the aircraft.

The fourth Convection and Moisture Experiment is sponsored by NASA's Earth
Science Enterprise. These investigations will be conducted in collaboration with the
National Oceanic and Atmospheric Administration's Hurricane Research Division and the
U.S. Weather Research Program. JPL is a division of the California Institute of
Technology in Pasadena.


August 16, 2001

BURST OF STAR FORMATION DRIVES BUBBLE IN GALAXY'S CORE

These NASA Hubble Space Telescope snapshots reveal dramatic
activities within the core of the galaxy NGC 3079, where a lumpy
bubble of hot gas is rising from a cauldron of glowing matter. The
picture at left shows the bubble in the center of the galaxy's disk.
The structure is more than 3,000 light-years wide and rises 3,500
light-years above the galaxy's disk. The smaller photo at right is a
close-up view of the bubble. Astronomers suspect that the bubble
is being blown by "winds" (high-speed streams of particles)
released during a burst of star formation. Gaseous filaments at the
top of the bubble are whirling around in a vortex and are being
expelled into space. Eventually, this gas will rain down upon the
galaxy's disk where it may collide with gas clouds, compress them,
and form a new generation of stars. The two white dots just above
the bubble are probably stars in the galaxy.

Credits: NASA, Gerald Cecil (University of North Carolina),
Sylvain Veilleux (University of Maryland), Joss Bland-Hawthorn
(Anglo- Australian Observatory), and Alex Filippenko (University of
California at Berkeley).

To see and read more, please click on:
http://oposite.stsci.edu/pubinfo/pr/2001/28 and links in
http://oposite.stsci.edu/pubinfo/latest.html
http://oposite.stsci.edu/pubinfo/pictures.html and
http://hubble.stsci.edu/go/news

The Space Telescope Science Institute (STScI) is operated by the
Association of Universities for Research in Astronomy, Inc. (AURA),
for NASA, under contract with the Goddard Space Flight Center,
Greenbelt, MD. The Hubble Space Telescope is a project of
international cooperation between NASA and the European Space
Agency (ESA).


H-Reflex Experiment on the International Space Station

Saint-Hubert, August 16, 2001- A second H-Reflex experiment will take place
today on the International Space Station.

Canadian scientist, Dr. Doug Watt of McGill University, is continuing his
research into the effects of microgravity on human reflexes. This research
has important implications for the health and safety of astronauts and may
also lead to improvements in managing balance disorders on earth,
particularly in the elderly.

For live coverage, media can log on to the NASA TV satellite on GE-2,
Transponder 9C at 85 degrees West longitude, vertical polarization, with a
frequency of 3880 MHz and audio of 6.8 MHz.
http://science.ksc.nasa.gov/shuttle/countdown/video/

REMINDER:

What: H-Reflex experiment on the International Space Station

When: Thursday, August 16 from 9:40am to 11:40am

Where: NASA TV

For more information on this experiment, visit the Canadian Space Agency web
site at
http://www.space.gc.ca or read the press release sent on Tuesday,
August 7th, 2001 at:
http://www.space.gc.ca/whatsnew/releases/pressrel/2001/010807.asp.


NOAA OFFICIALS DISCUSS HURRICANE MITCH RECONSTRUCTION PROJECT
Mark Completion of Life-Saving Central American Weather Forecast Effort

NOAA Officials will be available to discuss NOAA's $14 million effort to
put in place weather forecasting technology and infrastructure in Central
America to avert future tragedies brought on by hurricanes and severe
weather in the region. In 1998, Hurricane Mitch claimed 11,000 lives in
the region, making it the deadliest Atlantic hurricane in more than two
centuries. Interviews with NOAA and Central American government officials
and B-roll footage of will also be made available via satellite. The final
phase of NOAA's reconstruction project will be celebrated at a ceremony in
Managua, Nicaragua on August 22.

WHAT: Media Availability

WHERE: Teleconference

WHEN: Friday, August 17, 2001
10:30 a.m. - Noon; and 1:00 - 2:00 p.m.

WHO: Retired General Jack Kelly, director, National Weather Service
Gregory Withee, assistant administrator, NESDIS
Jamie Hawkins, deputy director, National Ocean Service

SATELLITE COORDINATES: Friday, August 17, 11:00 a.m. - 12:00 p.m. EDT
Transponder: PANAMSAT
Band: Ku
Downlink Frequency: 11921 MHz (h)
Audio 6.4 and 6.8
For more information about Hurricane Mitch and NOAA's reconstruction
program please visit: Hurricane Mitch Report -
http://www.nhc.noaa.gov/1998mitch.html
Hurricane Mitch satellite images -
http://www.ncdc.noaa.gov/ol/reports/mitch/mitch.html
NOAA GOES Homepage -
http://www.oso.noaa.gov/goes.


SPACE STATION PROGRAM REVIEW TEAM TO MEET AUG. 20-21;
REPORTERS INVITED TO ATTEND

The first meeting of the ISS Management and Cost
Evaluation Team is scheduled for Aug. 20-21 at NASA
Headquarters. The Aug. 20 session is open to the public, and
reporters are invited to attend.

During the Aug. 20 session, which begins at 8:30 a.m.,
Administration and NASA officials will provide a broad
overview of the Agency, the Human Exploration and Development
of Space Enterprise and the International Space Station
program.

The meeting will be held in conference room MIC-7, on the 7th
floor of the NASA Headquarters building. NASA Headquarters is
located at 300 E Street, SW, Washington, DC. Reporters
wishing to attend this session should call Kirsten Larson
(202/358-0243) or Ray Castillo (202/358-1600) to make the
necessary arrangements. Because of the small size of the
room, media television cameras will not be admitted to the
meeting.

NASA Administrator Daniel S. Goldin created the ISS
Management and Cost Evaluation Team last month to take a
focused look at the budget and management challenges facing
the International Space Station program.

Chaired by Thomas Young, the former president of Martin-
Marietta Corp., the task force will help NASA address the
quality of the ISS cost estimates as well as program
assumptions and requirements, identifying high-risk budget
areas and potential risk mitigation strategies.

The full membership of the panel can be found on the Internet
at:

ftp://ftp.hq.nasa.gov/pub/pao/pressrel/2001/01-152.txt


ISS Management and Cost Evaluation Task Force
August 20, 2001
NASA Headquarters

8:30 a.m. Panel Introductions
8:45 a.m. Opening Remarks Tom Young
Chairman

9 a.m. Welcome Daniel Goldin
NASA Administrator

9:30 a.m. Office of Management Sean O'Keefe
and Budget Perspective OMB Deputy Director

10 a.m. NASA Organization, Malcolm Peterson
Budget Overview NASA Comptroller

10:45 a.m. Break

11 a.m. Human Exploration and Joseph Rothenberg
Development of Space Associate Administrator
Office of Space Flight

Noon Lunch

1 p.m. ISS Facilities and Dr. Kathie Olsen
Research Chief Scientist

2 p.m. ISS Development Status Michael Hawes
Deputy Associate
Administrator,
Space Station
Office of Space Flight

3 p.m. Break

3:15 p.m. ISS-The Partners Angela Diaz
Director, Human Space
Flight and Research,
Office of External
Relations

4 p.m. Congressional TBD
Perspective NASA Legislative Affairs

5 p.m. Adjourn


X-43A MISHAP INVESTIGATION UPDATE

The board investigating the X-43A mission loss on June 2 is
continuing to meet at the Orbital Sciences Corp. facility in
Chandler, Ariz., where they relocated on June 24. Orbital is where
the Pegasus-derived booster rocket was built. The Pegasus was
attached to the X-43A to provide the boost to a predetermined
altitude.

The X-43A mission, first in a series of three, was lost moments after
the X-43A and its booster rocket were released from the wing of the
B-52 carrier aircraft. Following booster ignition, the combined
booster and X-43A experienced structural failure, deviated from its
flight path and was deliberately terminated.

Robert W. Hughes, the board chairman from Marshall Space Flight
Center, has said that the likelihood of finding a single root cause
of the mishap is still possible but becoming less probable. Hughes
restated that the investigation team was working to fully understand
the causal relationship and emphasized that the solution might
involve several contributing causes rather than a single cause.

To date, the team has closed approximately 85 percent of the fault
tree of several hundred possible or contributing causes. The
remaining potential causes, most dealing with launch vehicle control,
are being systematically investigated and evaluated.

The X-43A is designed to be the first scramjet-powered
aircraft, capable of attaining speeds as high as Mach 10.

NASA's Langley Research Center at Hampton, Va., leads the
X-43A program, with flight operations conducted by NASA Dryden Flight
Research Center, Edwards, Calif. Micro Craft, Inc., of Tullahoma,
Tenn., built the 12-foot-long X-43A vehicle. The mishap
investigation team includes representatives from NASA centers
including Dryden, Langley, Marshall (Alabama), Goddard (Maryland),
Kennedy (Florida), plus all of the contractor elements.


NASA selects Pace and Waite, Inc. for document services at Marshall Center

NASA has selected Pace and Waite, Inc., of Huntsville, AL, to
provide center-wide document services at NASA's Marshall Space Flight
Center, Huntsville, AL.

Under the contract, Pace and Waite will provide services for managing data
requirements, checking engineering drawings and operating the center's
documents release desk. Services to be provided are a continuation of an
effort currently being provided by Pace and Waite under a five-year contract
that ends this year.

The contract could have a potential value of approximately $39 million over
five years if all provisions are utilized. The cost-plus-incentive-fee
performance-based contract includes indefinite delivery/indefinite quantity
provisions. This contract will become effective Sept. 1, 2001, and includes
a one-year performance period plus four one-year priced options, which may
be exercised at NASA's discretion.

Marshall is NASA's lead center for development of space transportation and
propulsion systems. New technologies are being explored to make space more
accessible by reducing the cost of launching space vehicles while improving
flight safety. Marshall is also NASA's lead center for microgravity
research - conducting unique scientific studies in the near-weightlessness
of space to improve life on Earth.


SCIENTIFIC STUDY TRACKS GIANT BLUEFIN TUNAS ACROSS ATLANTIC
Research to help U.S. press for more effective international management

An independent study, funded in part by the Department of Commerce's
National Oceanic and Atmospheric Administration's (NOAA) National Marine
Fisheries Service (NOAA fisheries), improves scientists' understanding of
the migratory habits of one of the world's most valuable marine fish, the
Atlantic bluefin tuna. NOAA Fisheries managers believe the study, which
tracked giant bluefin tuna throughout the north Atlantic Ocean, provides
data which can strengthen international management measures.
The study reported in the August 17 issue of the journal Science, with
noted tuna researcher Dr. Barbara A. Block of Stanford University as lead
author, provides significant insight into the migration patterns of these
giant fish. This five year study was co-authored by Dr. Eric D. Prince of
NOAA Fisheries.

"The study confirms and expands on past migration-related traditional
tagging data and provides a wealth of new knowledge about the diving
patterns, thermal biology, feeding characteristics and environmental
preferences of Atlantic bluefin tuna," said Bill Hogarth, acting NOAA
fisheries director. "We are pleased to be a part of this important
research that gives scientists and managers a clearer picture of the
migratory, feeding and spawning habits of these fish."

Block and her team of researchers used two new state-of-the-art electronic
tags to monitor the movements of the fish. This group of scientists
assisted in the development of a new generation of electronic tags
initiated with a grant from NOAA fisheries. Using a combination of
satellite pop-up tags and archival tags, scientists were able to track the
tuna's migration and monitor several behavioral activities. More
information about the archival and pop-up tags is available at
http://www.montereybayaquarium.org/aa/aa_pressroom/aa_pkits_newsreleases.asp

NOAA fisheries managers are particularly interested in the newly reported
data because of their implications for future management decisions. An
accompanying article, also in the Aug. 17 journal Science, titled "Whose
fish are they anyway?" and co-authored by NOAA fisheries' Northeast
Fisheries Science Center director Dr. Michael Sissenwine, examines this
controversial marine fishery. Journalists may receive a copy by e-mail
from: scipak@aaas.org. Subscribers may access the article at
http://www.sciencemag.org. The public may obtain the article by calling
(202 326-6450.
Bluefin tuna in the Atlantic are highly sought after because they are
prized by recreational fishermen and they have a high commercial value in
Asian sushi and sashimi markets, with some fish going for as high as
$60,000. Harvesting of bluefin and other Atlantic tuna is managed through
catch quotas established by agreements of member countries through the
International Commission for the Conservation of Atlantic Tunas (ICCAT)
based in Madrid, Spain. Currently, bluefin tuna are managed as two
separate stocks, eastern and western. The western stock, the smaller of
the two, has tight restrictions placed on it. The larger eastern stock has
fewer restrictions. While scientists have been aware of mixing of the
stocks in international waters, where many countries fish, the nature of
mixing has not been well studied until now.

"The U.S. and its recreational and commercial fishing groups, along with
environmental and conservation organizations, has long supported the need
to rebuild Atlantic tunas through international agreement and compliance,"
said NOAA fisheries' Director of the Office of Habitat Conservation,
Rolland Schmitten, who is the U.S. ICCAT Commissioner. "We've seen that
effective science and management in the international arena have arrested
the decline of the western Atlantic bluefin tuna stock. The Block study is
a critical link in the knowledge we need to ultimately rebuild the stock
throughout the Atlantic. This science reaffirms that the level of harvest
of eastern Atlantic and Mediterranean bluefin tuna is excessive and must be
reduced, and that management measures in the east can affect the west."

At the request of the United States, ICCAT is already moving forward with
two stock mixing issues. ICCAT members have endorsed new research on
bluefin tuna in the central Atlantic to collect biological samples of
spawning size bluefin tuna in the Mid-Atlantic ocean to help determine if
there is a spawning area there. ICCAT scientists will review recent
studies, including the Block study, and prepare recommendations on how best
to account for the new mixing data on bluefin tuna in future stock
assessments and management decisions. Their recommendations will be
presented to the full ICCAT scientific body in October and to the ICCAT
commissioners in November.

In the Block study, researchers discovered that Atlantic bluefin often are
traveling throughout the entire North Atlantic and, in some cases, into the
Mediterranean Sea. Individual tuna also migrated from the Western Atlantic
to the east and back again in the same year. The Science article reported
that the western-tagged bluefin travel to distinct spawning grounds in the
Gulf of Mexico or the Eastern Mediterranean. "The results indicated that
western-tagged bluefin are vulnerable to fishing from all Atlantic bluefin
tuna fisheries," the authors report.

For more information about the Block study, go to:
http://www.stanford.edu/dept/news/report/

NOAA Fisheries is dedicated to protecting and preserving our nation's
living marine resources through scientific research, management,
enforcement, and the conservation of marine mammals and other protected
marine species and their habitat. To learn more about NOAA fisheries,
please visit
http://www.nmfs.noaa.gov


NASA SELECTS PACE AND WAITE, INC. FOR DOCUMENT SERVICES AT MARSHALL

NASA has selected Pace and Waite, Inc., of Huntsville, AL, to provide center-
wide document services at NASA's Marshall Space Flight Center, Huntsville, AL.

Under the contract, Pace and Waite will provide services for managing data
requirements, checking engineering drawings and operating the center's documents
release desk. Services to be provided are a continuation of an effort currently
being provided by Pace and Waite under a five-year contract that ends this year.

The contract could have a potential value of approximately $39 million over five
years if all provisions are utilized. The cost-plus-incentive-fee performance-
based contract includes indefinite delivery/indefinite quantity provisions.
This contract will become effective Sept. 1, 2001, and includes a one-year
performance period plus four one-year priced options, which may be exercised at
NASA's discretion.

Marshall is NASA's lead center for development of space transportation and
propulsion systems. New technologies are being explored to make space more
accessible by reducing the cost of launching space vehicles while improving
flight safety. Marshall is also NASA's lead center for microgravity research -
conducting unique scientific studies in the near-weightlessness of space to
improve life on Earth.



Table of Contents/AMERICAN GEOPHYSICAL UNION
============================================================================
1. NSF Information Technology Research Program Solicitation
2. Call for Papers for Fall 2001 AGU Special Session SM03: Electrodynamic
Coupling of High Latitude Ionosphere and Plasma Sheet (joint with SA, AE)
3. Job Announcement - Director of the Los Alamos National Laboratory (LANL)
Branch of the University of California (UC) Institute of Geophysics and
Planetary Physics (IGPP)
============================================================================
* Please direct all replies to editor@igpp.ucla.edu *
* !!!! DO NOT send any message to agu_spa@igpp.ucla.edu !!!! *
****************************************************************
SPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPA
*
* * * . . . . . . .
* * * AMERICAN GEOPHYSICAL UNION .
* ***** * . .. . . . . . . . .
* ********* * SPA SECTION NEWSLETTER . ..
*********** . . . . . . . .
* * *********** * * Volume VIII, Issue 83 . o .
*********** . . . . . . . .
* ********* * 15 August, 2001 . ..
* ***** * . .. . . . . . . . .
* * * Editor: Guan Le .
* * * Email: editor@igpp.ucla.edu . . . . . . .
*
SPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPASPA

-----------------------------------------------------------
1. NSF Information Technology Research Program Solicitation
-----------------------------------------------------------
From: "Baker, Kile B." <kbaker@nsf.gov>

The National Science Foundation has put the Program Solicitation for the
2001-2002 Information Technology Research program (NSF 01-149). You can
access the find the full Program Solicitation via the World Wide Web at
this URL:
http://www.nsf.gov/cgi-bin/getpub?nsf01149

The ITR program covers a broad area of science and technology. Proposals
are solicitied in three major classes, Large projects (proposals involving
multiple institutions with total budgets in the $5 - $15 Million range),
Medium (proposals with budgets in the $500 K - $5 M range), and Small
(budgets under $500 K total). The ATM division will be accepting proposals
in all classes, but the emphasis will be on proposals in the Medium class.

Although broad areas of science and technology are included in the ITR
program, the area of greatest interest to the ATM division will be
comprehensive models that may include ensemble forecasting, nesting and/or
data assimilation techniques to understand the complex interactions taking
place in the Earth system and provide better predictive capability of
phenomena ranging from natural hazards to biogeochemical cycles, space
weather and climate change; methods and co-laboratories for the integration
of heterogeneous environmental data sets from multiple observatories into
models.

Please note that Large class proposals require a pre-proposal. Please also
note the following deadlines:

Large projects: Pre-proposal deadline, Nov. 9, 2001;
full proposal deadline, .April 4, 2002.
Medium projects: Proposal deadline Nov. 13, 2001.
Small projects: Proposal deadline Feb. 6, 2002.

For more information on the ITR program as a whole, please consult the
Program Solicitation (NSF 01-149, see URL above). You will also find
additional information at the ITR web site, http://www.itr.nsf.gov. If you
would like more detailed information on the individual topics that will be
supported in the ATM division please contact the Program Director in the
area of your interest. You can find information about the various ATM
programs and contact information at
http://www.geo.nsf.gov/atm/.

----------------------------------------------------------------------------
2. Call for Papers for Fall 2001 AGU Special Session SM03: Electrodynamic
Coupling of High Latitude Ionosphere and Plasma Sheet (joint with SA, AE)
----------------------------------------------------------------------------
From: Vassilis Angelopoulos <vassilis@ssl.berkeley.edu>

Recent studies from the FAST, POLAR and Geotail spacecraft have revealed that
copious amounts of electromagnetic energy flux propagate down the field lines
from the nightside plasma sheet in the form of dissipative Alfven waves.
Space imagers have shown that the increased Alfvenic wave power correlates
with the poleward motion of active aurorae, or activations of the poleward
boundary, while in situ, low altitude measurements suggest that upward
ion beams and counterstreaming electron events are observed at high intensity
on the same field lines. Fast flows emanating from reconnection, or other
near-Earth processes, provide ample free energy for the aforementioned waves.
This session addresses the electromagnetic coupling of plasma sheet activations
with the high latitude ionosphere. In particular, Alfven wave generation,
propagation, and dissipation along (or at the ionospheric foot of)
the field lines is or primary interest. The effect of the waves on
ion and electron populations, the ionospheric closure of the pertinent
current, and the effective damping of the ultimate source are themes
of importance. Recent Cluster auroral zone field line traversals
at various altitudes also provide a unique multi-spacecraft viewpoint
which is particularly interesting and timely. Observational, simulation
and theory papers are encouraged.

Conveners: *V. Angelopoulos, Space Sciences Laboratory, University of
California, Berkeley, CA 94720-7450; tel: 510-643-1871, fax: 510-643-8302,
E-mail: vassilis@ssl.berkeley.edu; and J. R. Wygant, University of
Minnesota, Tate Laboratory of Physics, School of Physics and Astronomy,
116 Church Street, SE, Minneapolis, MN 55455-0112, tel: 612-626-8921
fax: 612-626-2029, Email: wygant@ham.space.umn.edu

INVITED SPEAKERS (Tentative Theme):

C. W. Carlson (Auroral observations of high latitude processes and possible
mapping to plasma sheet)
A. Keiling (The high latitude aurora seen from POLAR altitudes, sources
and sinks of plasma sheet energy)
R. Nakamura (Plasma sheet processes resulting in field-aligned
energy flux generation; the source region)
W. Lotko (Wave generation and dissipation along field lines leading to
high latitude auroral forms).

---------------------------------------------------------------------------
3. Job Announcement - Director of the Los Alamos National Laboratory (LANL)
Branch of the University of California (UC) Institute of Geophysics and
Planetary Physics (IGPP)
---------------------------------------------------------------------------
From: "Bruce L. Barraclough" <bbarraclough@lanl.gov>

Summary: The Los Alamos branch of the Institute of Geophysics and
Planetary Physics (IGPP) is searching for a Director. This Center at Los
Alamos is a branch of a University of California multi-campus research
unit with a mission to foster and sponsor collaborative research in solid
earth geophysics, geochemistry, hydrology, planetary geophysics,
astrophysics, ocean/atmospheric, and magnetospheric sciences and other
geophysical and planetary phenomena between the Los Alamos National
Laboratory, the University of California and other universities. The IGPP
Director provides scientific/technical leadership and line management of
IGPP. The Los Alamos National Laboratory is managed by the University of
California for the U.S. Department of Energy. Collaborations between the
Laboratory and the University are very important to the intellectual
vitality of the Laboratory, and the IGPP Director serves to foster such
collaborations in the scientific areas mentioned above. The branch funds
a range of collaborative projects involving Laboratory and University
investigators. The Director will be responsible for overseeing a yearly
peer-review process to select proposals for funding. The Institute hosts
visiting scholars, post doctoral fellows, and graduate students for short
and long-term visits. Organizationally, the Institute is located within
the Earth and Environmental Sciences (EES) Division that is within the
Strategic and Supporting Research Directorate at Los Alamos. IGPP plays
an institutional role within the Laboratory and encourages collaboration
with scientists throughout the entire Laboratory. The Director of IGPP at
Los Alamos is expected to develop and lead a coordinated program that
will target and create cooperative basic research programs. The Director
is expected to guide long-term research activities that are consistent
with the Laboratory's policies for funding discretionary research. The
Director is expected to develop a strong working relationship with the
IGPP External Advisory Committee as well as plans to implement their
recommendations. While it is expected that the majority of the
Director's time will be devoted to the tasks above, the opportunity for
individual research by the Director is negotiable. The Director's line
management responsibility includes accountability for the quality of
research; strategic planning; development and maintenance of technical
capabilities; environment, safety and health; security; workforce
excellence, productivity, and diversity; financial management; cost
effectiveness; and communications. The IGPP Director must maintain
effective working relationships with leaders, managers, and staff
throughout the Laboratory, government, university, and industrial
officials and collaborators.

Required Skills:
* Demonstrated successful experience in one of the following
disciplines: solid earth geophysics, geochemistry, hydrology,
planetary geophysics, astrophysics, ocean/atmospheric sciences,
magnetospheric sciences, mineral physics, or other related scientific
areas.
* Demonstrated success in management of personnel in a scientific
organization, including effective management of resources.
* Successful experience establishing and maintaining research
collaborations.
* Experience and accomplishments in strategic and tactical planning and
in leading execution of the plans.
* Ability to balance competing interests with available resources and
establish clear priorities and focus.
* Track record of commitment to responsible and high-quality
operations, including safety, environmental protection, and security.
* Demonstrated effective interpersonal skills, including uncompromising
honesty and integrity; and ability to earn the respect of
subordinates, supervisors, peers, and customers.
* Record of effective two-way written and oral communications skills,
as evidenced by internal and external interactions, including
briefings, presentation, publications, and meetings.
* Ability to obtain a Q clearance.
Desired Skills:
* Detailed knowledge of the Laboratory, the University, DOE, and other
national and international programs of relevance to the Center%92s
activities.
* Experience with the management and administration systems and
practices of national laboratories and/or UC universities.
Education: Ph.D. degree in a scientific or engineering field relevant to
IGPP or equivalent combination of education and experience.

Job Number: 017583
Title: CENTER LEADER Number of Openings: 1
Series/Level: TSM MGT Recruiting Scope: Open to all
Organization: EES-DO Status: Open
Date Posted: 07/17/2001 Job Type: Regular Full-time
Clearance: Q (Position will be cleared to this level). Applicants
selected will be subject to a Federal background
investigation and must meet eligibility requirements for
access to classified matter.
Notes to Applicants: For specific questions about the status of this
job, call (505) 665-9955 .


John Bluck

Aug. 15, 2001
NASA Ames Research Center, Moffett Field, CA

NASA PAO on duty
NASA Newsroom, Jacksonville Naval Air Station, FL

RELEASE: 01-59AR
NASA AMES COORDINATES HUGE HURRICANE OBSERVATION CAMPAIGN

Learning how to increase the warning time before Atlantic hurricanes make
landfall is a goal of some100 U.S. researchers from NASA and other agencies
who will a begin a 5-week campaign on Aug. 16.

Airborne researchers will fly above, around and through these weather
monsters, and also will use satellites, balloons, unpiloted aircraft and
ground-based instruments to gather hurricane data. Scientists from five
NASA centers, several government agencies and 10 universities are
cooperating to study tropical storms that erupt in the Atlantic Ocean.

"The Ames Earth Science Project Office is coordinating and managing the
overall project," said Steve Hipskind, project manager at NASA's Ames
Research Center in California's Silicon Valley. Called the Fourth
Convection And Moisture EXperiment (CAMEX-4), the scientific campaign
begins Aug. 16 with a 'media day' for journalists at Jacksonville Naval Air
Station, FL. The project is scheduled to last until Sept. 24.

A major campaign goal is to produce more accurate hurricane predictions of
storm landfall to decrease the size of coastal evacuations and to increase
warning time. Researchers also are striving to reduce landfall track and
intensity forecast errors and improve precipitation forecasts to enable
more accurate inland flooding predictions.

"We will be making measurements in hurricanes with the NASA DC-8 and ER-2
aircraft out of Jacksonville Naval Air Station, FL," Hipskind said. "In
addition, we will be flying a low-altitude uninhabited aerial vehicle
(drone airplane), the Aerosonde. There will be ground instrumentation
(several large weather radar and balloon soundings), as well as a large
theoretical and satellite science team. Our collaborators include the
National Oceanic and Atmospheric Administration (NOAA) and Air Force
'Hurricane Hunters,' both of which provide operational aircraft
reconnaissance in hurricanes, as well as the NOAA Hurricane Research
Division and the United States Weather Research Program." The National
Science Foundation is providing researchers from the National Center for
Atmospheric Research for the campaign.

Mike Craig of Ames is sharing project management responsibility with
Hipskind. Craig is doing much of the planning with Hipskind and taking the
field lead for the second half of the deployment. The large team of
researchers will select hurricanes and study them as they approach landfall
in the Caribbean, Gulf of Mexico and along the East Coast of the United
States. Aircraft operations will be within a 1,725-mile radius (2,760 km)
of Jacksonville.


CAMEX-4 is focussed on the study of hurricane development, tracking,
intensification and landfall impacts using NASA-funded aircraft and surface
remote instruments. When possible, scientists will compare and validate
measurements with coincident observations from the QuikSCAT, Terra and
Tropical Rainfall Measuring Mission satellites. This study will yield high
spacial and temporal information of hurricane structure, dynamics and
motion. Scientists want to capture two complete "snapshots" of a hurricane.

The resulting data -- when analyzed within the context of more traditional
aircraft, satellite and ground-based radar observations -- should provide
additional insight to hurricane modelers and forecasters who strive to
improve hurricane predictions.

NASA Ames is responsible for assuring the airworthiness and flight safety
of the remotely piloted Aerosonde aircraft, and the overall operational
readiness and collaborative agreements for all of the participating
aircraft, according to Hipskind. Each Aerosonde weighs about 30 pounds
(less than 15 kg) and will fly between 500 ft. and 1,500 ft. (150 m - 450
m) in the hurricane's winds to gather data and send it back to researchers.
Should one of the tiny uninhabited aircraft be sucked up to higher
altitudes, controllers would send a signal to destroy it to avoid a
collision with another aircraft.

"Ames also has participating scientists," Hipskind said. "Paul Bui is the
principal investigator for the meteorological measurement system for the
DC-8 aircraft, and Lenny Pfister is the co-investigator on both Paul's
experiment, as well as a NASA Jet Propulsion Laboratory (Pasadena, CA)
laser hygrometer on the DC-8." A hygrometer is an instrument that measures
humidity in the air.

Bui's experiment includes three major systems on the DC-8 airplane that
normally flies at a medium altitude between 20,000 ft. and 40,000 ft. (
6,000 m - 12,000 m). The systems will measure air velocity to give
scientists a three-dimensional picture of wind directions. Bui also will
provide extremely accurate temperature measurements, critical to
understanding details of hurricane cloud formation.

While remote sensing of the hurricane environment is the primary objective
of CAMEX-4, separate flights will study thunderstorm structure,
precipitation systems and atmospheric water vapor profiles. The objective
of these flights is to improve precipitation estimates from microwave
instruments, particularly to validate NASA satellite measurements.

The NASA Earth Science Enterprise sponsors CAMEX-4. More CAMEX-4
information is on the Internet at:
http://www.hurricanes.nasa.gov and
http://camex.msfc.nasa.gov


John Bluck

Aug. 15, 2001
NASA Ames Research Center, Moffett Field, CA
Phone: 650/604-5026 or 650/604-9000
e-mail: jbluck@mail.arc.nasa.gov

NASA PAO on duty
NASA Newsroom, Jacksonville Naval Air Station, FL
Phone: 904/542-3846
E-mail: david.steitz@hq.nasa.gov

RELEASE: 01-59AR

NASA AMES COORDINATES HUGE HURRICANE OBSERVATION CAMPAIGN

Learning how to increase the warning time before Atlantic hurricanes make
landfall is a goal of some100 U.S. researchers from NASA and other agencies
who will a begin a 5-week campaign on Aug. 16.

Airborne researchers will fly above, around and through these weather
monsters, and also will use satellites, balloons, unpiloted aircraft and
ground-based instruments to gather hurricane data. Scientists from five
NASA centers, several government agencies and 10 universities are
cooperating to study tropical storms that erupt in the Atlantic Ocean.

"The Ames Earth Science Project Office is coordinating and managing the
overall project," said Steve Hipskind, project manager at NASA's Ames
Research Center in California's Silicon Valley. Called the Fourth
Convection And Moisture EXperiment (CAMEX-4), the scientific campaign
begins Aug. 16 with a 'media day' for journalists at Jacksonville Naval Air
Station, FL. The project is scheduled to last until Sept. 24.

A major campaign goal is to produce more accurate hurricane predictions of
storm landfall to decrease the size of coastal evacuations and to increase
warning time. Researchers also are striving to reduce landfall track and
intensity forecast errors and improve precipitation forecasts to enable
more accurate inland flooding predictions.

"We will be making measurements in hurricanes with the NASA DC-8 and ER-2
aircraft out of Jacksonville Naval Air Station, FL," Hipskind said. "In
addition, we will be flying a low-altitude uninhabited aerial vehicle
(drone airplane), the Aerosonde. There will be ground instrumentation
(several large weather radar and balloon soundings), as well as a large
theoretical and satellite science team. Our collaborators include the
National Oceanic and Atmospheric Administration (NOAA) and Air Force
'Hurricane Hunters,' both of which provide operational aircraft
reconnaissance in hurricanes, as well as the NOAA Hurricane Research
Division and the United States Weather Research Program." The National
Science Foundation is providing researchers from the National Center for
Atmospheric Research for the campaign.

Mike Craig of Ames is sharing project management responsibility with
Hipskind. Craig is doing much of the planning with Hipskind and taking the
field lead for the second half of the deployment. The large team of
researchers will select hurricanes and study them as they approach landfall
in the Caribbean, Gulf of Mexico and along the East Coast of the United
States. Aircraft operations will be within a 1,725-mile radius (2,760 km)
of Jacksonville.

-more-
-2-
CAMEX-4 is focussed on the study of hurricane development, tracking,
intensification and landfall impacts using NASA-funded aircraft and surface
remote instruments. When possible, scientists will compare and validate
measurements with coincident observations from the QuikSCAT, Terra and
Tropical Rainfall Measuring Mission satellites. This study will yield high
spacial and temporal information of hurricane structure, dynamics and
motion. Scientists want to capture two complete "snapshots" of a hurricane.

The resulting data -- when analyzed within the context of more traditional
aircraft, satellite and ground-based radar observations -- should provide
additional insight to hurricane modelers and forecasters who strive to
improve hurricane predictions.

NASA Ames is responsible for assuring the airworthiness and flight safety
of the remotely piloted Aerosonde aircraft, and the overall operational
readiness and collaborative agreements for all of the participating
aircraft, according to Hipskind. Each Aerosonde weighs about 30 pounds
(less than 15 kg) and will fly between 500 ft. and 1,500 ft. (150 m - 450
m) in the hurricane's winds to gather data and send it back to researchers.
Should one of the tiny uninhabited aircraft be sucked up to higher
altitudes, controllers would send a signal to destroy it to avoid a
collision with another aircraft.

"Ames also has participating scientists," Hipskind said. "Paul Bui is the
principal investigator for the meteorological measurement system for the
DC-8 aircraft, and Lenny Pfister is the co-investigator on both Paul's
experiment, as well as a NASA Jet Propulsion Laboratory (Pasadena, CA)
laser hygrometer on the DC-8." A hygrometer is an instrument that measures
humidity in the air.

Bui's experiment includes three major systems on the DC-8 airplane that
normally flies at a medium altitude between 20,000 ft. and 40,000 ft. (
6,000 m - 12,000 m). The systems will measure air velocity to give
scientists a three-dimensional picture of wind directions. Bui also will
provide extremely accurate temperature measurements, critical to
understanding details of hurricane cloud formation.

While remote sensing of the hurricane environment is the primary objective
of CAMEX-4, separate flights will study thunderstorm structure,
precipitation systems and atmospheric water vapor profiles. The objective
of these flights is to improve precipitation estimates from microwave
instruments, particularly to validate NASA satellite measurements.

The NASA Earth Science Enterprise sponsors CAMEX-4. More CAMEX-4
information is on the Internet at: http://www.hurricanes.nasa.gov and
http://camex.msfc.nasa.gov

Steve Roy
Marshall Space Flight Center, Huntsville, Ala.

RELEASE No: 01-59

NASA BRAVES STORMS IN QUEST FOR BETTER UNDERSTANDING OF HURRICANES

As this year's hurricane season arrives, a team of researchers
participating in a NASA study is ready. Armed with airplanes from
NASA's Dryden Flight Research Center, Edwards, Calif., robotic aerial
vehicles and a fleet of sophisticated instruments, the researchers
are ready to meet these potentially deadly and destructive storms
head-on, gathering data vital to improve hurricane modeling and
prediction.

They are taking part in the Convection And Moisture Experiment
(CAMEX) - the fourth in a series of field investigations sponsored by
the Earth Science Enterprise at NASA Headquarters, Washington D.C.
The mission unites researchers from 10 universities, five NASA
centers and the National Oceanic and Atmospheric Administration
(NOAA).

Based out of the Naval Air Station at Jacksonville, Fla., this year's
mission takes place Aug. 16 through Sept. 24 - traditionally the most
active part of the hurricane season. During CAMEX, researchers will
gather storm data from multiple sources, including aircraft,
unpiloted aerial vehicles, satellite observations, ground-based radar
and other sensing instruments. Unique in this mission is the fact
that each storm will be monitored simultaneously from near sea level
to 65,000 feet.

Temperature, pressure, humidity, precipitation, wind speed, ice
crystal sizes, and lightning characteristics are examples of the
kinds of information that will be collected. These data are expected
to provide additional insight to hurricane researchers and
forecasters who continually strive to improve hurricane predictions.

"One reason NASA studies hurricanes is to understand the best way to
use information from NASA resources, such as its satellites, to
provide better warnings to the American public and people around the
world affected by hurricanes," said Robbie Hood, CAMEX mission
scientist from NASA's Marshall Space Flight Center, Huntsville, Ala.

"During the last CAMEX experiment in 1998, we flew over hurricanes
and collected a vast amount of data, sampling the hurricanes' upper
regions at altitudes of 35,000 feet or higher," said Hood. "This year,
we're asking ourselves additional questions, such as, 'How does a
hurricane intensify?' and "What is its rainfall potential after it
comes to shore?' The highest number of hurricane-related deaths are
due to inland flooding, so inland rainfall is something we will be
monitoring very closely."

NASA Dryden's ER-2 and DC-8 will fly into the season's hurricanes
carrying a suite of scientific instruments to study selected storms
as they approach landfall in the Caribbean, Gulf of Mexico and along
the East Coast of the United States.

The DC-8, equipped with instruments that will measure the storms'
structure, environment and changes in intensity and tracking, will
fly into storms at 35,000 to 40,000 feet. At the same time, the
specially equipped ER-2, a high-altitude research aircraft, will soar
above storms at 65,000 feet.

Although investigating hurricanes is the primary objective of
CAMEX-4, separate flights will study thunderstorm structure,
precipitation systems and atmospheric water vapor profiles. This
portion of CAMEX-4 is known as Keys Area Microphysics Project (KAMP).
The project seeks improved precipitation estimates from passive and
active microwave instruments - equipment that detects precipitation
and surface water by measuring natural microwave emissions from cloud
water, cloud ice, rainfall and surface water. Flights for the
microphysics project will take place in the area of Key West, Fla.

CAMEX-4 is part of NASA's Earth Science Enterprise, a long-term
research program dedicated to better understanding the total Earth
system and the effects of natural and human-induced changes on the
global environment.


Donald Savage
Headquarters, Washington

Amber Jones
National Science Foundation, Arlington, VA
RELEASE: 01-166

ASTRONOMERS FIND JUPITER-SIZED
PLANET ORBITING STAR IN BIG DIPPER

A team of astronomers has found a Jupiter-sized planet
orbiting a faint nearby star similar to our Sun, raising
intriguing prospects of finding a solar system like our own.

The planet is the second found orbiting the star 47 Ursae
Majoris in the Big Dipper, also known as Ursa Major or the
Big Bear. The new planet is at least three-fourths the mass
of Jupiter and orbits the star at a distance that, in our
Solar System, would place it beyond Mars but within the orbit
of Jupiter.

"Astronomers have detected evidence of more than 70
extrasolar planets," said Morris Aizenman, a senior science
advisor at the National Science Foundation (NSF). "Each
discovery brings us closer to determining whether other
planetary systems have features like those of our own."

"For the first time we have detected two planets in nearly
circular orbits around the same star," said team member Debra
Fischer of the University of California at Berkeley. "Most
of the 70 planets people we have found to date are in bizarre
solar systems, with short periods and eccentric orbits close
to the star. As our sensitivity improves we are finally
seeing planets with longer orbital periods, planetary systems
that look more like our Solar System."

The planet-search team, which is supported by NASA and the
National Science Foundation, Arlington, VA, has been
instrumental in finding a majority of the planets outside our
Solar System (also called extrasolar planets). Besides
Fischer, the team includes Geoffrey Marcy, also of Berkeley,
Paul Butler of the Carnegie Institution of Washington, Steve
Vogt of the University of California at Santa Cruz and
Gregory Laughlin of NASA's Ames Research Center, Mountain
View, CA. Their report on the new planet has been submitted
to the Astrophysical Journal.

A few years ago, Marcy and Butler discovered a planet more
than twice the mass of Jupiter in a circular orbit around the
same star. The star is one of 100 that the scientists have
targeted since 1987 in their search for evidence of
extrasolar planets. Using telescopes at the University of
California's Lick Observatory, they measure changes in the
characteristics of light emitted by the stars. Those changes,
they believe, signal the presence of a planet periodically
pulling the star toward or away from Earth.

Fischer was able to see the periodic wobble from the second
planet, smaller and farther from the star than the first,
because of improved instrumentation.

The star is a yellow star similar to the sun, probably about
seven billion years old and located about 51 light-years from
Earth. A light-year, the distance light travels in one year,
is approximately 6 trillion miles.

"Every new planetary system reveals some new quirk that we
didn't expect. We've found planets in small orbits and wacky
eccentric orbits," said Marcy. "With 47 Ursae Majoris, it's
heartwarming to find a planetary system that finally reminds
us of our solar system."


Samples of the Future

The advanced space ships of tomorrow will be crafted from far-out
materials with extraordinary resistance to the harsh environment of space.
An experiment strapped to the outside of the ISS aims to put such
materials through their paces.

FULL STORY at

http://science.nasa.gov/headlines/y2001/ast15aug_1.htm?list448368


August 15, 2001

National Aeronautics and
Space Administration
Dryden Flight Research Center
Edwards, California 93523

For Release: August 14, 2001

Mike Braukus
NASA Headquarters

Frederick A. Johnsen, News Chief
NASA Dryden Flight Research Center

RELEASE No: 01-58

NASA SOLAR AIRCRAFT SETS ALTITUDE RECORD;
COMMUNICATIONS AND ENVIRONMENTAL BREAKTHROUGHS EXPECTED

A new world record altitude of 96,500 feet over the Pacific Ocean was
reached by the solar-powered Helios Prototype flying wing at 4:08
p.m. Hawaii Standard Time (HST), Aug. 13, fulfilling the expectations
of engineers from NASA's Dryden Flight Research Center and
AeroVironment, Inc., builders of the 247-ft. wing. This is the first
time a non-rocket powered aircraft has maintained flight this far
above the earth. Sustained operations at that altitude promise to
enable capabilities ranging from environmental monitoring to
radically improved communications on earth to simulating flight in
the atmosphere of Mars.

Daniel S. Goldin, NASA Administrator, who has been a strong supporter
of solar powered flight, said, "This is a ground breaking
accomplishment which will advance this technology to new heights."

The remotely-piloted wing took off from the U.S. Navy's Pacific
Missile Range Facility on the Hawaiian island of Kauai at 8:48 a.m.
HST. Flying at about 25 miles an hour, the mission lasted nearly 17
hours, landing at 1:43 a.m. Aug. 14.

The record flight sets the stage for follow-on missions that will use
a regenerative fuel system now under development to enable Helios to
remain aloft 24 hours a day for months at a time. The record
altitude was achieved during daylight hours, relying on solar cells
on the wing's surface to provide electrical power. Descent after
dark was possible as the 14 electric motors were no longer needed to
maintain altitude. During descent the propellers acted as generators,
providing electrical power to control the aircraft.

"This is like going to the Olympics and setting a new world record
for engineers," said NASA Dryden Flight Research Center solar
aircraft project manager John Del Frate. "This achievement did not
come easily. Thousands of things had to work right for something
like this to come together."

Production variants of Helios might see service as long-term earth
environmental monitors, as well as communications relays, reducing
dependence on satellites and providing service in areas not covered
by satellites. The successful flight at high altitude also provides
NASA with information about flight on Mars, since the atmosphere at
that height above earth replicates the atmosphere near the Martian
surface.


Mike Braukus
Headquarters, Washington

Frederick A. Johnsen
Dryden Flight Research Center, Edwards, CA

RELEASE: 01-165

NASA SOLAR AIRCRAFT SETS ALTITUDE RECORD; COMMUNICATIONS,
ENVIRONMENTAL BREAKTHROUGHS EXPECTED

NASA's solar-powered, propeller-driven Helios aircraft
set a new world record altitude of 96,500 feet on Monday,
surpassing the old record for aircraft without rocket power
by more than 10,000 feet. Sustained operations at that
altitude promise to enable capabilities ranging from
environmental monitoring to radically improved communications
on Earth to simulating flight in the atmosphere of Mars.

NASA Adminstrator Daniel S. Goldin, who has been a strong
supporter of solar-powered flight, said, "This is a ground
breaking accomplishment which will advance this technology to
new heights."

The remotely piloted wing, built by AeroVironment, Inc.,
Monrovia, CA, took off from the U.S. Navy's Pacific Missile
Range Facility on the Hawaiian island of Kauai at 8:48 a.m.
local time. Flying at about 25 miles an hour, the aircraft
stayed aloft almost 17 hours, passing the old altitude
records of 80,200 feet for propeller-driven aircraft and
85,068 feet for any aircraft not powered by rockets. Helios
reached its highest altitude at 4:08 p.m. local time and
landed at 1:43 a.m. Tuesday local time.

The record flight sets the stage for follow-on missions that
will use a regenerative fuel system now under development to
enable Helios to remain aloft 24 hours a day for months at a
time. The aircraft reached record altitude during daylight
hours, relying on solar cells on the wing's surface to
provide electrical power. Descent after dark was possible as
the 14 electric motors were no longer needed to maintain
altitude. During descent the propellers acted as generators,
providing electrical power to control the aircraft.

Production variants of Helios might see service as long-term
Earth environmental monitors or as communications relays,
reducing dependence on satellites and providing service in
areas not covered by satellites. The successful flight at
high altitude also provides NASA with information about
flight on Mars, since the atmosphere at that height above
Earth replicates the atmosphere near the Martian surface.


August 14, 2001

David E. Steitz
Headquarters, Washington

Steve Roy
Marshall Space Flight Center, Huntsville, AL

Bill Dougherty
Office of Public Affairs, Naval Air Station, Jacksonville,
FL

NOTE TO EDITORS: N01-046

NASA HURRICANE MISSION BRIEFING ON AUG. 16 IN JACKSONVILLE,
FL

NASA will kick off the fourth Convection and Moisture
Experiment (CAMEX-4) during a press conference and aircraft
tour at the Naval Air Station (NAS) Jacksonville, FL, on
Thursday, Aug. 16, at 9 a.m. EDT. Media wishing to attend
the press conference should meet at the Yorktown Gate of NAS
Jacksonville no later than 8:30 a.m. for escort to the
briefing room. Following the briefing, media will be
escorted to the airfield to view the NASA DC-8 and ER-2
research aircraft, as well as the remotely piloted Aerosonde
aircraft, and other planes involved in the mission.

Based out of NAS Jacksonville, this year's mission will run
from Aug. 16 through Sept. 24 - traditionally the most
active part of the hurricane season. During CAMEX,
researchers will gather storm data from multiple sources,
including piloted aircraft, remotely piloted aerial
vehicles, satellite observations, ground-based radar, and
other ground-based sensing instruments.

CAMEX-4 is the latest in a series of field research
investigations sponsored by the Earth Sciences Enterprise at
NASA Headquarters in Washington, DC. It unites researchers
from 10 universities, five NASA centers and the National
Oceanic and Atmospheric Administration (NOAA).

For more information about the CAMEX field campaign, please
see:

http://camex.msfc.nasa.gov

http://www.earth.nasa.gov


Dancing around the Black Hole

recent observations with the infrared-sensitive ISAAC instrument on the
VLT ANTU telescope have allowed a team of French and Swiss astronomers
to obtain measurements of stars that move very close to the central
black holes in some active galaxies. They were surprised to find signs
of the presence of young stars in this area. The full story is available
as ESO PR 18/01 at URL:

http://www.eso.org/outreach/press-rel/pr-2001/pr-18-01.html

Other, recent observations with the VLT concern the spectrum of (one of)
the most distant objects known, a quasar with redshift 6.3. Details have
been published in a Press Release by the Max-Planck-Society, available
on the web at:

http://www.mpg.de/pri01/pri0152.htm

("Juengster Quasar durchleuchtet Urmaterie des Universums" - in German).

Important message to media representatives:

Please note that two international Press Conferences on the subjects of
"Black Holes" and "Exoplanets" will be held in conjunction with the
upcoming JENAM conference in Munich (Germany) on September 11 and 12,
respectively. Full information is available at:

http://www.eso.org/outreach/pr-events/


August 13, 2001

This Week on Galileo
August 10 - 19, 2001

With the hectic activity of the Io encounter now behind it, Galileo settles
into the more peaceful pace of orbital cruise. But first, the last bit of
cleanup from the flyby must be taken care of. On Friday, August 10, the
spacecraft executes an orbit trim maneuver. This engine burn will correct
any remaining uncertainties or errors in the flyby path, and begin to nudge
the spacecraft towards its next target. That target once again is Io, which
we will pass in mid-October.

On Saturday the spacecraft again uses its thrusters, this time to turn in
place and point the antenna closer to the Earth. This 4 degree turn takes
about 10 minutes to perform. On Sunday, routine maintenance of the
propulsion system is performed. This will guarantee that all parts of the
propulsion system are properly exercised, not just those branches that are
used for the particular maneuvers and turns we have done recently.

In addition to these navigation and engineering tasks, playback of the
science data from last weekend's flyby continues. A quick survey of the
data on the tape takes up the first week or so of playback. Due to the
effects of the accumulated radiation the spacecraft has received in its
nearly six years in orbit around Jupiter, measurements from several
instruments have been affected. The survey will determine if any of the
data on the tape are bad, and allow the scientists to plan how best to
retrieve the good data on subsequent passes over the tape.

For more information on the Galileo spacecraft and its mission to Jupiter,
please visit the Galileo home page at one of the following URL's:

http://galileo.jpl.nasa.gov
http://www.jpl.nasa.gov/galileo


NASA Marshall Space Flight Center
Huntsville, Ala. 35812

RELEASE: 01-275

NASA study to brave storms in quest for better prediction, understanding of
hurricanes

As this year's hurricane season rolls in, a team of researchers
participating in a NASA study is waiting. Armed with airplanes, robotic
aerial vehicles and a fleet of sophisticated instruments, they're ready to
meet these potentially deadly and destructive storms head-on, gathering data
vital to improve hurricane modeling and prediction.

They're part of the Convection And Moisture EXperiment (CAMEX) --
the fourth in a series of field research investigations sponsored by the
Earth Science Enterprise at NASA Headquarters, Washington, DC. The mission
unites researchers from 10 universities, five NASA centers and the National
Oceanic and Atmospheric Administration (NOAA).

Based out of the Naval Air Station at Jacksonville, Fla., this
year's mission will run from Aug. 16 through Sept. 24 -- traditionally the
most active part of the hurricane season.

During CAMEX, researchers will gather storm data from multiple
sources, including aircraft, unpiloted aerial vehicles, satellite
observations, ground-based radar, and other ground-based sensing
instruments. Unique in this mission is the fact each storm will be monitored
simultaneously from near sea level to 65,000 feet.

Temperature, pressure, humidity, precipitation, wind speed,
lightning and ice crystal sizes are examples of the kinds of information
that will be collected. These data are expected to provide additional
insight to hurricane researchers and forecasters who continually strive to
improve our understanding of these storms.

"One reason NASA studies hurricanes is to understand the best way to
use information from NASA resources, such as its satellites, to provide
better warnings to the American public and people around the world affected
by hurricanes," said Robbie Hood, CAMEX mission scientist from NASA's
Marshall Space Flight Center, Huntsville, Ala.

"During the last CAMEX mission in 1998, we flew over hurricanes and
collected a vast amount of data, sampling the hurricanes' upper regions at
altitudes of 35,000 feet (10,600 meters) or higher," said Hood. "This year,
we're asking ourselves additional questions, such as, 'How does a hurricane
intensify?' and 'What is its rainfall potential after it comes to shore?'
The highest number of hurricane-related deaths are due to inland flooding,
so inland rainfall is something we will be monitoring very closely."

The CAMEX team plans to fly into the season's hurricanes aboard two
NASA planes, the ER-2 and DC-8, both from NASA's Dryden Flight Research
Center, Edwards, Calif. Carrying a series of instruments, these aircraft
will fly over, through, and around selected hurricanes as they approach
landfall in the Caribbean, Gulf of Mexico, and along the East Coast of the
United States.

The DC-8, equipped with instruments that will measure the storms'
structure, environment and changes in intensity and tracking, will fly into
storms at 35,000 to 40,000 feet (12,200 meters). At the same time, the
specially equipped ER-2, a high-altitude research plane, will soar above
storms at 65,000 feet (19,800 meters).

NASA also is funding the flight of several unpiloted aerial vehicles
called the Aerosonde Robotic Aircraft, managed in conjunction with the
University of Colorado at Boulder.

Small, robotic aircraft designed for collection of meteorological
data over oceans and remote areas, the Aerosondes will operate over the
North Atlantic Ocean taking observations in the lower atmosphere. In the
first use of unpiloted aircraft in an operation of this type, the Aerosondes
will skim the ocean surface collecting data on atmospheric temperature,
pressure, relative humidity, and winds ­ data that cannot be obtained by any
other method.

Although investigating hurricanes is the primary objective of
CAMEX-4, separate flights will study thunderstorm structure, precipitation
systems, and atmospheric water vapor profiles.

This portion of CAMEX-4 is known as Keys Area Microphysics Project
(KAMP). The project seeks improved precipitation estimates from passive and
active microwave instruments ­ equipment that detects precipitation and
surface water by measuring natural microwave emissions from cloud water,
cloud ice, rainfall and surface water. Flights for the microphysics project
will be approximately 300 nautical miles (560 km) from the Key West, Fla.,
area.

The hurricane study is part of NASA's Earth Science Enterprise, a
long-term research program dedicated to better understanding the total Earth
system and the effects of natural and human-induced changes on our global
environment.


NASA Marshall Space Flight Center
Huntsville, Ala. 35812

RELEASE: 01-275

NASA study to brave storms in quest for better prediction, understanding of
hurricanes

As this year's hurricane season rolls in, a team of researchers
participating in a NASA study is waiting. Armed with airplanes, robotic
aerial vehicles and a fleet of sophisticated instruments, they're ready to
meet these potentially deadly and destructive storms head-on, gathering data
vital to improve hurricane modeling and prediction.

They're part of the Convection And Moisture EXperiment (CAMEX) --
the fourth in a series of field research investigations sponsored by the
Earth Science Enterprise at NASA Headquarters, Washington, DC. The mission
unites researchers from 10 universities, five NASA centers and the National
Oceanic and Atmospheric Administration (NOAA).

Based out of the Naval Air Station at Jacksonville, Fla., this
year's mission will run from Aug. 16 through Sept. 24 -- traditionally the
most active part of the hurricane season.

During CAMEX, researchers will gather storm data from multiple
sources, including aircraft, unpiloted aerial vehicles, satellite
observations, ground-based radar, and other ground-based sensing
instruments. Unique in this mission is the fact each storm will be monitored
simultaneously from near sea level to 65,000 feet.

Temperature, pressure, humidity, precipitation, wind speed,
lightning and ice crystal sizes are examples of the kinds of information
that will be collected. These data are expected to provide additional
insight to hurricane researchers and forecasters who continually strive to
improve our understanding of these storms.

"One reason NASA studies hurricanes is to understand the best way to
use information from NASA resources, such as its satellites, to provide
better warnings to the American public and people around the world affected
by hurricanes," said Robbie Hood, CAMEX mission scientist from NASA's
Marshall Space Flight Center, Huntsville, Ala.

"During the last CAMEX mission in 1998, we flew over hurricanes and
collected a vast amount of data, sampling the hurricanes' upper regions at
altitudes of 35,000 feet (10,600 meters) or higher," said Hood. "This year,
we're asking ourselves additional questions, such as, 'How does a hurricane
intensify?' and 'What is its rainfall potential after it comes to shore?'
The highest number of hurricane-related deaths are due to inland flooding,
so inland rainfall is something we will be monitoring very closely."

The CAMEX team plans to fly into the season's hurricanes aboard two
NASA planes, the ER-2 and DC-8, both from NASA's Dryden Flight Research
Center, Edwards, Calif. Carrying a series of instruments, these aircraft
will fly over, through, and around selected hurricanes as they approach
landfall in the Caribbean, Gulf of Mexico, and along the East Coast of the
United States.

The DC-8, equipped with instruments that will measure the storms'
structure, environment and changes in intensity and tracking, will fly into
storms at 35,000 to 40,000 feet (12,200 meters). At the same time, the
specially equipped ER-2, a high-altitude research plane, will soar above
storms at 65,000 feet (19,800 meters).

NASA also is funding the flight of several unpiloted aerial vehicles
called the Aerosonde Robotic Aircraft, managed in conjunction with the
University of Colorado at Boulder.

Small, robotic aircraft designed for collection of meteorological
data over oceans and remote areas, the Aerosondes will operate over the
North Atlantic Ocean taking observations in the lower atmosphere. In the
first use of unpiloted aircraft in an operation of this type, the Aerosondes
will skim the ocean surface collecting data on atmospheric temperature,
pressure, relative humidity, and winds ­ data that cannot be obtained by any
other method.

Although investigating hurricanes is the primary objective of
CAMEX-4, separate flights will study thunderstorm structure, precipitation
systems, and atmospheric water vapor profiles.

This portion of CAMEX-4 is known as Keys Area Microphysics Project
(KAMP). The project seeks improved precipitation estimates from passive and
active microwave instruments ­ equipment that detects precipitation and
surface water by measuring natural microwave emissions from cloud water,
cloud ice, rainfall and surface water. Flights for the microphysics project
will be approximately 300 nautical miles (560 km) from the Key West, Fla.,
area.

The hurricane study is part of NASA's Earth Science Enterprise, a
long-term research program dedicated to better understanding the total Earth
system and the effects of natural and human-induced changes on our global
environment.


Exploring Mars: Blowing in the Wind?

One answer to roving across the surface of Mars may be blowing in the wind.
Literally.

Researchers exploring different methods to deliver scientific instruments to
various Martian locales are studying the potential for a giant, lightweight,
two-story tall beach ball. Equipped with scientific instruments, the
so-called "tumbleweed ball" conceived by JPL researchers could potentially
explore vast tracts of planetary terrain, blown by the wind.

The wind blowing across the face of the red planet would be the only engine
needed to move the giant tumbleweed ball from place to place, said Jack A.Jones,

who is leading JPL's research into various inflatable machines for
exploring space. JPL's Inflatable Technology for Robotics Program aims to
create rugged, all-terrain vehicles and other devices with low mass and
low-packing volume.

A scientific payload, carrying instruments such as magnetometers or
water-seeking radar, would be held in place by tension cords at the
tumbleweed's center. Cameras mounted inside the ball would peer out at the
local terrain. When scientists identify a promising spot and want the
tumbleweed to put down roots and sit for a spell, the ball could be
partially deflated. Then, when it's time to move along again, the ball could
be reinflated to roll on toward new frontiers.

"This is preliminary work," Jones admonishes as he prepares for more field
tests. But he is enthusiastic about the promise this technology may hold for
the exploration of Mars and other solar system bodies.

Much of Mars' terrain is sloping and littered with boulders, which makes
tough going for most vehicles. But researchers were excited by the results
of tests this summer of a 1.5 meter-tall version of the tumbleweed. The
tests confirmed that 6-meter diameter (about 20-feet) balls should be able
to climb over or around one-meter rocks and travel up slopes as high as
25-degrees in the thin, but breezy martian air.

Follow the Bouncing Ball

Serendipity and a busted wheel on an experimental rover played a roll in
planting the idea that would grow into the tumbleweed ball.

Previous tests of beach ball-size tumbleweed prototypes had been
disappointing. "They got stuck," Jones explained. Driven by the wind, the
toy-size balls lodged against knee- and waist-high rocks like those that
dominate much of Mars' terrain. As rovers, the beach balls flopped.

But then, while conducting tests of an experimental inflatable rover in the
Mojave Desert's Dumont Dunes, one of the bright yellow rover's shoulder-high
spherical "tires" broke off the vehicle and blew away.

"It went a quarter of a mile in nothing flat," recalled technician Tim
Connors, who quickly saddled up with the driver of a passing all-terrain
recreational vehicle to chase down the runaway sphere. The moderate, 20-mile
per hour afternoon winds drove the ball fast and far.

"It soared," Jones said of the big ball. Watching Connors in hot pursuit,
the researchers marveled at the speed of the rogue sphere and the ease with
which it moved across the desert, unimpeded by boulders. "Tim was flying
over the sand dunes trying to catch it," he said. "The ball went up steep,
steep cliffs of sand. Nothing stopped it." Until Connors, on the borrowed
ATV, was able to catch up and corral the escapee.

"And therein was planted the seed," said Jones, "that if we make these
things big enough, nothing will stop one."

Toys, Balloons, and Serious Science

In a lab that appears to mix three parts of serious R&D to one part of
Santa's festive workshop, Jones and his colleagues are surrounded by shiny
Mylar balloons of various sizes, pink and yellow beach balls, heavy-duty
nylon tumbleweed ball prototypes, tall tanks of compressed gas and
worktables full of mechanical and electronic devices. The team, which
includes senior engineer Sam Kim and design engineer Jay Wu is now preparing
for desert tests later this month that will incorporate a radar into the
ball's center to test the prototype's ability to find underground water.
Such instrumentation could eventually be used to search for possible water
hidden beneath Mars' surface.

The ball is weighted so that it has a preferred axis of rotation. It tends
to roll with the heaviest part down, so two weights opposite each other send
the ball along a straight path. The upcoming tests will also try out a
center-of-mass control device that Connors conceived of which would allow
the ball to be steered by pumping contained fluid to the left, right or
center of the tire, which will be slightly oblong.

"Again, this is experimental, so we're trying different things," said Jones.
"But I'm pretty confident it will work."

"With a 20 kilogram ball and 20 kilogram payload, the 6-meter diameter
tumbleweed ball is light enough that it could be added on to another lander
and deployed from the ground, or it could be in its own delivery vehicle,"
said Jones. The large, lightweight ball could possibly also serve as its own
parachute and landing airbag, he said, able to withstand the bounce
following a 30-meter per second terminal velocity descent at Mars. The ball
itself shares the same heritage as the airbag used for Pathfinder and that
which will be used for the Mars Exploration Rover.

Upcoming Tests

Other work being planned for coming months include desert drop tests with a
prototype tumbleweed ball made of super rugged Vectran, the same material
used for the Mars Pathfinder's airbag landing system. In the coming year,
Jones hopes to arrange for long-range testing of hundreds or thousands of
kilometers in the harsh, challenging, Marslike environment of the Arctic or
Antarctic.


RELEASE: 01-58AR

AMES COMPLETES SUCCESSFUL TEST OF MARS AIRPLANE PROTOTYPE

Soaring gracefully down to Earth from a balloon floating 101,000 feet high
above Oregon, a NASA prototype of an airplane that someday may fly over
Mars successfully completed a high-altitude flight test this week.

Conducted at Oregon's Tillamook airport by the Kitty Hawk 3 project at NASA
Ames Research Center, Moffett Field, CA, the test was designed to validate
the aerodynamic performance of the prototype. Nicknamed "Orville" after
one of the famed Wright brothers who first flew on Dec. 17, 1903, the NASA
731 glider was dropped from a helium-filled balloon that towed it up to an
altitude of 101,000 feet - the highest ever for such a test - before
releasing it. Engineers and scientists hailed the test as a great success.

"It was a great flight and everything went really well. It appears that we
realized all of our test objectives," exclaimed a jubilant Andy Gonzales,
an Ames aerospace engineer who served as the flight test director.
Low-altitude tests of NASA 729, another prototype called "Wilbur," were
conducted last month at Ames.

"Mars has always fascinated people," said Larry Lemke, an aerospace
engineer at NASA Ames who serves as Ames' project manager for advanced Mars
mobility concepts, which include airplanes as well as other systems.
"Every time we send a mission up there, we come back with fascinating
discoveries."

According to Lemke, a Mars airplane is an idea whose time has come. "The
Mars airplane is an idea that has been around for about 25 years, and over
the past five years or so, it has been growing in popularity," he said. "I
think a Mars airplane will play a role in exploring the Red Planet."

Conventional in appearance, the Mars airplane concept developed by Ames
engineers features a long, straight wing and twin tails in the rear. The
remote-controlled glider tested in Oregon featured an approximately
four-foot-long fuselage and an eight-foot wing span.

"The flying we have successfully completed in Oregon is very similar to the
flying that we will be doing over Mars during a productive exploration
mission," Lemke said. "One unique aspect of flying a Mars mission with an
airplane is that it must be constructed in a fold-up configuration in order
to fit inside a spacecraft."

In its future configuration for Mars, the aircraft is expected to have its
own propeller propulsion system capable of operating in the Mars
atmosphere, which is comprised mostly of carbon dioxide. It will also
carry a variety of sophisticated instruments to observe and conduct science
experiments.

"The possibility of life on Mars is a very hot topic and an interesting
question, so I'm sure you will find instruments on board that are designed
to find signs of water on Mars, which is necessary for life," Lemke said.

"In addition, we would have a large array of cameras on the airplane to be
able to see large areas of the Mars terrain in very high resolution," Lemke
said. He said the cameras aboard the aircraft would be so precise, they
could see objects on Mars as small as the size of a quarter. "I think the
images will be stunning," he said. "During a Mars airplane mission, we will
be able to view the planet at very close proximity and this will convey to
the public that there is a real planet there, not just an abstract."

"Our test flight at Tillamook airport showed the airplane's flight was very
smooth and stable which makes for a good platform for science instruments,"
said Gonzales.

Ames engineers predict the next few years will be challenging, as they
prepare for a potential mission to Mars. "We will be expanding the envelope
and developing a much more complex aircraft for exploring Mars," Lemke
said. The next step will be to develop a Mars airplane model with folding
wings and later, one with a propeller propulsion system.


NASA STUDY TO BRAVE STORMS IN QUEST FOR
BETTER PREDICTION, UNDERSTANDING OF HURRICANES

As this year's hurricane season rolls in, a team of
researchers participating in a NASA study is waiting. Armed
with airplanes, robotic aerial vehicles and a fleet of
sophisticated instruments, they're ready to meet these
potentially deadly and destructive storms head-on, gathering
data vital to improve hurricane modeling and prediction.

They're part of the Convection And Moisture EXperiment
(CAMEX) -- the fourth in a series of field research
investigations sponsored by the Earth Science Enterprise at
NASA Headquarters, Washington, DC. The mission unites
researchers from 10 universities, five NASA centers and the
National Oceanic and Atmospheric Administration (NOAA).

Based out of the Naval Air Station at Jacksonville, FL., this
year's mission will run from Aug. 16 through Sept. 24 ­
traditionally the most active part of the hurricane season.
During CAMEX, researchers will gather storm data from
multiple sources, including aircraft, unpiloted aerial
vehicles, satellite observations, ground-based radar, and
other ground-based sensing instruments. Unique in this
mission is the fact each storm will be monitored
simultaneously from near sea level to 65,000 feet.

Temperature, pressure, humidity, precipitation, wind speed,
lightning and ice crystal sizes are examples of the kinds of
information that will be collected. These data are expected
to provide additional insight to hurricane researchers and
forecasters who continually strive to improve our
understanding of these storms.

"One reason NASA studies hurricanes is to understand the best
way to use information from NASA resources, such as its
satellites, to provide better warnings to the American public
and people around the world affected by hurricanes," said
Robbie Hood, CAMEX mission scientist from NASA's Marshall
Space Flight Center, Huntsville, AL.

"During the last CAMEX mission in 1998, we flew over
hurricanes and collected a vast amount of data, sampling the
hurricanes' upper regions at altitudes of 35,000 feet (10,600
meters) or higher," said Hood. "This year, we're asking
ourselves additional questions, such as, 'How does a
hurricane intensify?' and 'What is its rainfall potential
after it comes to shore?' The highest number of hurricane-
related deaths are due to inland flooding, so inland rainfall
is something we will be monitoring very closely."

The CAMEX team plans to fly into the season's hurricanes
aboard two NASA planes, the ER-2 and DC-8, both from NASA's
Dryden Flight Research Center, Edwards, CA. Carrying a series
of instruments, these aircraft will fly over, through, and
around selected hurricanes as they approach landfall in the
Caribbean, Gulf of Mexico, and along the East Coast of the
United States.

The DC-8, equipped with instruments that will measure the
storms' structure, environment and changes in intensity and
tracking, will fly into storms at 35,000 to 40,000 feet
(12,200 meters). At the same time, the specially equipped
ER-2, a high-altitude research plane, will soar above storms
at 65,000 feet (19,800 meters).

NASA also is funding the flight of several unpiloted aerial
vehicles called the Aerosonde Robotic Aircraft, managed in
conjunction with the University of Colorado at Boulder.
Small, robotic aircraft designed for collection of
meteorological data over oceans and remote areas, the
Aerosondes will operate over the North Atlantic Ocean taking
observations in the lower atmosphere. In the first use of
unpiloted aircraft in an operation of this type, the
Aerosondes will skim the ocean surface collecting data on
atmospheric temperature, pressure, relative humidity, and
winds ­ data that cannot be obtained by any other method.

Although investigating hurricanes is the primary objective of
CAMEX-4, separate flights will study thunderstorm structure,
precipitation systems, and atmospheric water vapor profiles.

This portion of CAMEX-4 is known as Keys Area Microphysics
Project (KAMP). The project seeks improved precipitation
estimates from passive and active microwave instruments ­
equipment that detects precipitation and surface water by
measuring natural microwave emissions from cloud water, cloud
ice, rainfall and surface water. Flights for the microphysics
project will be approximately 300 nautical miles (560 km)
from the Key West, FL area.

The hurricane study is part of NASA's Earth Science
Enterprise, a long-term research program dedicated to better
understanding the total Earth system and the effects of
natural and human-induced changes on our global environment.

August 11, 2001

JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIFORNIA 91109.

GENESIS MISSION STATUS
Friday, August 10, 2001-
Photos & Art work By: NASA

Two days after launch from Cape Canaveral, Fla., the
Genesis mission continues to proceed exceedingly well.
Since the spacecraft's signal was acquired by a Deep
Space Network ground station at Goldstone, Calif., at 10:38
p.m. PDT on Wednesday, Aug. 8, the mission team has continued
to monitor the status of spacecraft subsystems. All of them
are performing normally. Ground controllers established a two-
way communication link between Genesis and Earth, enabling the
navigation team to start collecting data to assess the
spacecraft's flight path.

Genesis' flight path was adjusted successfully today at
about 10:21 a.m. PDT. The small thrusters burned for 53.5
seconds. This moved the spacecraft about 5.2 meters per
second (11.6 miles per hour) into a path to reach the Lagrange
1, or L1, point, where the gravities of the Sun and Earth are
balanced. Genesis will reach L1 in November 2001. The
navigation team expects to be able to determine by Monday how
to modify the spacecraft's flight path during the next
adjustment in early September.

Among various housekeeping events just after launch, the
team commanded the spacecraft to transmit to Earth and brought
the spacecraft out of safe mode. Safe mode is a standby state
used to keep the spacecraft dormant during launch. Genesis
has now communicated with all three of NASA's Deep Space
Network stations -- in Goldstone, Calif.; Canberra, Australia;
and Madrid, Spain.

The team also commanded Genesis to spin at its normal
rate, 1.6 revolutions per minute.
Genesis will collect pieces of the Sun called solar wind
to help scientists better understand our solar system's
development.

JPL, a division of the California Institute of
Technology, manages the Genesis mission for NASA's Office of
Space Science, Washington, D.C. Lockheed Martin Astronautics,
Denver, Colo., designed and built the spacecraft and will
operate it jointly with JPL. Major portions of the payload
design and fabrication were carried out at the Los Alamos
National Laboratory in New Mexico and at NASA's Johnson Space
Center, Houston, Texas.


August 10, 2001

Horse Flies and Meteors

Like bugs streaking down the side window of a moving car, long and
colorful Perseid Earthgrazers could put on a remarkable show before
midnight on August 11th.

FULL STORY at

http://science.nasa.gov/headlines/y2001/ast09aug_1.htm?list448368


EDUCATORS LEARN ABOUT THE INS AND OUTS OF THE SOLAR SYTEM

Educators from around the country are studying such NASA
missions as 2001 Mars Odyssey, currently en route to the red
planet, during an institute sponsored by NASA's Jet Propulsion
Laboratory in Pasadena, from Aug. 9 to 11.

Thirty-three educators are participating in the Solar
System Educator Program Institute. Most are teachers from
kindergarten through high school levels. Others are from
museums, science centers or planetariums. All of them come
with a strong background in teaching science or math and a
passion for training teachers.

This nationwide network of highly motivated educators is
at the heart of the program. Each educator agrees to lead at
least three workshops per year in their home states. Over the
course of a year, the program trains thousands of educators,
teaching them ways to incorporate space education into their
lesson plans.

"The program goal is to inspire America's students,
create learning opportunities and enlighten inquisitive minds
by engaging them in the planetary exploration efforts
conducted by JPL," said Terri Formico, program coordinator at
JPL.

More information is available at http://www.ssep.org/ .

Space Explorers Inc. and the Virginia Space Grant
Consortium manage the program for JPL.
NASA/JPL missions and programs participating in the institute
include the Cassini mission to Saturn, the Stardust and Deep
Impact comet missions, the Galileo mission to Jupiter, the
Mars Exploration Program, the Outer Planets program and Europa
Orbiter mission and the Deep Space Network of ground-based
antennas that communicate with spacecraft, the JPL Education
and Public Outreach Office and NASA's Solar System Exploration
Education and Public Outreach Forum.


Karen Horting
Science's Next Wave, Washington

RELEASE: 01-162

NASA PROVIDES "SCIENCE'S NEXT WAVE" FOR MINORITY SCHOOLS

As part of its ongoing commitment to education, NASA has
teamed with the journal Science to provide Historically Black
Colleges and Universities (HBCUs) in the Leadership Alliance
access to a weekly on-line publication devoted to scientific
training and career development.

The online publication, "Science's Next Wave," provides
global news, profiles of emerging careers, and advice from
experts in the scientific community at large. Next Wave is a
global source of information that is updated weekly and can
be accessed 24 hours a day, 7 days a week, from the Internet.

"This resource was initially provided to NASA employees. With
the assistance of George Reese, Associate Administrator for
Equal Opportunity Programs, we decided to extend the program
to include HBCUs when we realized what a great opportunity
this could be to link the best and brightest minds to
promising careers in science. We hope that the subscription
will inform as well as encourage students, especially
minorities, to pursue science-related career opportunities
that are available," said Dr. Kathie Olsen, NASA Chief
Scientist and Acting Associate Administrator for Biological
and Physical Research at NASA Headquarters in Washington.

The subscription will cover the minority schools in the
Leadership Alliance, including: Clark Atlanta University,
Delaware State University, Howard University, Morehouse
College, Morgan State University, Prairie View A&M
University, Southern University at Baton Rouge, Spelman
College, Tougaloo University, Xavier University, and the
University of Puerto Rico system.

"Sadly, the number of underrepresented minorities receiving
graduate degrees in the sciences is still extremely low. For
this reason, we are heartened by NASA's commitment to make
the training and mentoring of underrepresented minority
science students a top priority," said Ellis Rubinstein,
editor of Science.

Some of the resources that will be available to the students
are the Career Development Center for Postdocs and Junior
Faculty, the Grant Doctor, and the new Postdoc Network.
These features provide information for beginning scientists,
tips on writing grants and locating funds, help with time
management, and question-and-answer sessions.

More information on "Next Wave" or the Leadership Alliance
can be found at:

http://www.nextwave.org

http://www.leadershipalliance.org


NASA Ames Research Center, Moffett Field, CA

RELEASE: 01-57AR

SAN JOSE HIGH SCHOOL WINS NATIONAL ROBOTICS CONTEST FOR 2ND YEAR

A San Jose 'continuation' high school team has won a national robotics competition for the second year in a row, this time in Seattle.

On Wednesday, Foothill High School won the 2001 National Botball Tournament in Seattle at the American Association of Artificial Intelligence conference. Botball is a robotics sport for which students construct and compete autonomous LEGO robots that manipulate objects on a tabletop.

"Here we have the kids that society expects the worst of, and they give us their absolute best," said mentor Alan Federman, an engineer at NASA Ames Research Center in California's Silicon Valley. "I am very proud of this school. Nobody has ever won two consecutive national robotics contests," he said. Last year, Foothill students were leaders of the championship alliance of the 2000 FIRST Robotics Tournament in Orlando, FL. In the Orlando contest, students constructed a large, remote-control robot entirely different from this year's botball model.

"After that Foothill win in 2000, a lot of people thought it was a fluke, something that could never happen again in a million years," Federman said.

Foothill's students, mostly of Hispanic or Asian heritage, sometimes are classified as 'youth at risk.' For the robotics work, they must understand basic principals of engineering and computer programming.

Foothill teacher Jeneva Westendorf assisted the student team. NASA Ames engineer Terry Grant mentored team members. In addition, former NASA engineer Jeff Ota, a member of the East Side Union District High School board, was involved in the project.

Forty-seven student teams from across the nation competed in this year's botball tournament in Seattle. Three other schools from the East Side Union High School District in San Jose also took part and did well in this year's competition. These schools are Andrew Hill High School, Overfelt High School and Independence High School.

The NASA Robotics Education Project assists students in learning engineering and computer skills by supporting the botball competition and other educational robotics activities.

Additional information is on the Internet at: http://robotics.nasa.gov and at: http://www.kipr.org



NOAA HURRICANE SCIENTISTS TEST NEW FORECAST DEVICES
DURING TROPICAL STORM BARRY

             Even though Tropical Storm Barry's winds were a few miles an hour shy of
hurricane strength, the storm gave hurricane researchers at the Commerce
Department's National Oceanic and Atmospheric Administration (NOAA) several
opportunities to test new technology that may tell them more about wind
speed changes and landfall characteristics of tropical cyclones.


Hurricane researchers at NOAA's Atlantic Oceanographic and Meteorological
Laboratory (AOML), supporting the U. S. Weather Research Program (USWRP),
are working closely with NOAA's National Hurricane Center (NHC) to develop
new techniques that will provide a better understanding of wind structure
and storm intensity changes, plus valuable information on storm track
guidance.

Dr. Hugh Willoughby, director of AOML's Hurricane Research Division said,
"The real accomplishment this summer is the closer connection between
ground-breaking research and practical forecasting that benefits every
coastal resident in harm's way."

Knowing wind speed at ground level when a hurricane makes landfall is of
paramount importance to local emergency management personnel. To provide
that information, meteorologists at AOML have created H*Wind, a program
that visually depicts the wind speeds and denotes in easy-to-read color
bands the regions of hurricane and gale force winds around a storm.
Hurricane specialists at the hurricane center tried their hand at running
H*Wind for the first time during Tropical Storm Barry, focusing on timely
analysis and quality control of real-time wind observations. H*Wind is
also being used in a post-storm analysis to determine Barry's actual wind
speed at landfall.

Being able to accurately predict where a tropical cyclone will make
landfall is another key factor to forecasters. For the best measurements,
hurricane researchers have developed a technique that identifies the "sweet
spots" in a storm that will yield the most accurate data. Scientists on
board NOAA's hurricane surveillance Gulfstream-IV jet used the technique to
take measurements of Tropical Storm Barry. Those measurements were
incorporated in the models that the National Hurricane Center specialists
used to issue landfall forecasts. It is anticipated this technique will
provide nearly 15 percent improvement in the landfall forecast when fully
operational.

For more information about NOAA's hurricane research mentioned in this
press release, please visit the following sites:
http://www.aoml.noaa.gov/hrd/assessment/
http://www.aoml.noaa.gov/hrd/Storm_pages/wind.html
http://www.aoml.noaa.gov/hrd/HFP2001/
http://www.aoml.noaa.gov/hrd/project2000/jk_proj2.html

For more information on NOAA's National Hurricane Center, please visit:
http://www.nhc.noaa.gov

For more information on NOAA's Aircraft Operations Center, please visit:
http://www.omao.noaa.gov//aoc/index.html



Kirsten Larson
Headquarters, Washington

Susan Hendrix
Goddard Space Flight Center, Greenbelt, MD

RELEASE: 01-163

NASA TO ACCEPT TDRS-H COMMUNICATION SATELLITE

Boeing Satellite Systems, El Segundo, CA, has completed
the verification and checkout process for the Boeing-built
Tracking and Data Relay Satellite, TDRS-H, launched June
2000. NASA and Boeing are finalizing conditions for
acceptance of TDRS-H, and negotiations are expected to
conclude in late August.

Upon acceptance of the TDRS-H spacecraft, NASA's existing
fleet will expand to seven on-orbit spacecraft. The agency
will move the TDRS-H to its operational location at 171
degrees West longitude in September and rename it TDRS-8. The
spacecraft then will be ready to serve the scientific
community for years to come.

TDRS-H soon will be joined by TDRS-I and -J. TDRS-I is
scheduled to launch Oct. 29 aboard an Atlas IIA rocket from
Cape Canaveral Air Force Station, FL, at 11:14 p.m. EST, and
TDRS-J will launch in October 2002. Once in place, the three
next-generation satellites will double the capacity of data
transmission and will provide nearly continuous, high-
bandwidth communications links between Earth and space for
the International Space Station, Space Shuttle and a host of
near-Earth orbiting space research missions into the next
decade.

NASA's acceptance of TDRS-H has been delayed due to a
performance shortfall on the Multiple-Access (MA) phased
array antenna aboard the spacecraft. During on-orbit testing
in August 2000, Boeing Satellite Systems, Inc., discovered
that the MA communication services were performing at less-
than-specified capability. All other communications services,
including the newly added Ka-band single-access services,
have been activated and tested and are performing well.

"Boeing has been extremely responsive since the problem was
first identified," said Robert Spearing, Deputy Associate
Administrator for Space Communications at NASA Headquarters.
"Launching TDRS-H ahead of actual need, gave us time to
identify any shortcomings and address them successfully
before there was an impact on our customers."

"We are convinced that Boeing understands the most probable
root cause of the underperformance and has taken the
necessary actions to prevent any such shortfall from
occurring on TDRS-I and -J," said TDRS Project Manager Robert
Jenkens Jr. of NASA's Goddard Space Flight Center in
Greenbelt, MD. Boeing has modified and tested TDRS-I and -J
to ensure optimal performance.

The TDRS satellite fleet relays large volumes of data --
including voice, television and scientific information --
from human-rated vehicles or orbiting scientific spacecraft
back to control centers on the ground. Aside from providing
near-continuous coverage for human space missions, the next-
generation TDRS spacecraft will relay data from the Hubble
Space Telescope, Tropical Rainfall Measuring Mission, LANDSAT
and the Earth Observing System. The spacecraft also provide
expendable-launch-vehicle tracking services to launch service
providers.


NEW VIEW OF PRIMORDIAL HELIUM TRACES THE STRUCTURE
OF EARLY UNIVERSE

NASA's Far Ultraviolet Spectroscopic Explorer (FUSE) satellite has
given astronomers their best glimpse yet at the ghostly cobweb of
helium gas left over from the big bang, which underlies the universe's
structure. The helium is not found in galaxies or stars but spread
thinly through the vastness of space. The helium traces the
architecture of the universe back to very early times. This
structure arose from small gravitational instabilities seeded in
the chaos just after the big bang. These FUSE observations help
confirm theoretical models of how matter in the expanding universe
condensed into a web-like structure pervading all of the space
between galaxies.

The FUSE is a NASA Origins mission developed and operated by
The Johns Hopkins University in collaboration with NASA's
Goddard Space Flight Center, the Centre National d'Etudes Spatiales
(France), the Canadian Space Agency, the University of Colorado,
and the University of California, Berkeley. FUSE was launched on
June 24, 1999 on a three-year mission to obtain high-resolution
spectra in the far ultraviolet wavelength region (905-1185 Angstroms)
of faint galactic and extragalactic objects. For further information
about FUSE, visit the mission web site at
http://fuse.pha.jhu.edu.

To see and read more, please click on
http://oposite.stsci.edu/pubinfo/pr/2001/27 or links in
http://hubble.stsci.edu/go/news
http://oposite.stsci.edu/pubinfo/latest.html and
http://oposite.stsci.edu/pubinfo/pictures.html

The Space Telescope Science Institute (STScI) is operated by the
Association of Universities for Research in Astronomy, Inc. (AURA),
for NASA, under contract with the Goddard Space Flight Center,
Greenbelt, MD. The Hubble Space Telescope is a project of
international cooperation between NASA and the European Space
Agency (ESA).


HELIOS PROTOTYPE TO ATTEMPT RECORD FLIGHT THIS WEEKEND

A new world's altitude record for a non-rocket-powered
aircraft could be achieved over Hawaii this weekend by the
NASA-sponsored Helios Prototype solar-electric flying wing. The
flight from the U.S. Navy's Pacific Missile Range Facility (PMRF) on
the island of Kauai is tentatively set for Saturday, Aug. 11, with
backup flight days scheduled for Aug. 12 and 13, and Aug. 16 through
19.
The Helios Prototype is believed capable of reaching
altitudes in the vicinity of 100,000 feet under ideal conditions.
Engineers estimate the aircraft could reach at least 95,000 feet on
this mission with 100,000 feet still a possibility, well above the
current record of 85,068 feet for sustained horizontal flight set by
a SR-71 in 1966.
Designed and built by AeroVironment, Inc., of Monrovia,
Calif., the ultra-lightweight Helios Prototype's development is
funded and managed under NASA's Environmental Research Aircraft and
Sensor Technology (ERAST) project. The demonstration flight should
validate the Helios' capability as a platform for high-altitude
environmental monitoring and atmospheric sampling missions
.


NASA SCIENTIST TO SPEAK SATURDAY AT THE TECH MUSEUM

Dr. Charles Wade, senior staff scientist in the Life Sciences Division at NASA's Ames Research Center,

will speak at The Tech Museum of Innovation in San Jose on Saturday, Aug.11, at 2 p.m. in the Center for Learning.

Wade's talk is titled "Altered gravity and life processes: building habitats for living systems on the International Space Station.

" Ames' Space Station Biological Research Project (SSBRP) is leading NASA's efforts to develop the systems required to support

a wide range of fundamental gravitational biology research on the International Space Station. SSBRP manages the

development of several habitats that will provide life support, environmental control, and monitoring

systems for various research subjects and specimens, including plants, cells, eggs, insects, aquatic species and rodents.

Scientists in Ames' Life Sciences Division study how the unique environment of space affects living systems,

from cells in culture to physiological studies in animals and humans. Through a better understanding of

fundamental physiology will come knowledge useful for both the maintenance of human health on

Earth and the development of countermeasures to the effects of long-term space flight.

The division conducts ground-based life sciences research, and implements flight experiments

onboard the space shuttle, the International Space Station, and a variety of unpiloted international

spacecraft. It also develops the technology required to perform life sciences research on the ground

and in space and works to transfer technology and promote education to improve the quality of

life on Earth. More information is available at: http://lifesci.arc.nasa.gov/

Life sciences research at Ames is supported by NASA's Office of Biological and

Physical Research, which promotes basic and applied research to support human exploration

of space and to take advantage of the space environment as a laboratory. More information is available at: http://spaceresearch.nasa.gov/

The Tech Museum is an educational resource designed to engage people of all ages and backgrounds

in exploring and experiencing technologies affecting their lives, and to inspire young people to become

innovators in developing the technologies of the future. More information is available at: www.thetech.org


Cassini Weekly Significant Events
for 08/02/01 - 08/08/01

The most recent spacecraft telemetry was acquired from the Madrid tracking
station on Wednesday, August 8. The Cassini spacecraft is in an excellent
state of health and is operating normally. Information on the
spacecraft's position and speed can be viewed on the "Present Position"
web page,
http://www.jpl.nasa.gov/cassini/english/where/ .

Recent spacecraft activities include the conclusion of a Magnetospheric
and Plasma Science observation, a Radio and Plasma Wave Science (RPWS)
High Frequency Receiver Calibration, powering off the Composite Infrared
Spectrometer, and an autonomous memory load partition repair of Solid
State Recorder-B.

The third and final of the instrument muting tests was completed this
week. This test puts Cassini in a position to perform future Probe
Checkouts with the instruments placed in a sleep state and having their
Bus Interface Unit's transmission port 'muted'. Prior to these tests,
Probe Checkouts required the Cassini instruments to be powered off for the
duration of the activity. This new capability will allow the instruments
to avoid incurring an undesired cycle as they are powered off and on again.

In support of the C28 sequence process, the "b" version of the C28
sequence products was released, as was the draft package for the
Preliminary Sequence Integration and Validation meeting. A meeting was
held to define the Integration Test Laboratory (ITL) simulation support
for Flight Software Normalization activities for the Cosmic Dust Analyzer
(CDA) and Visual and Infrared Mapping Spectrometer. Also discussed were
the results of the successful instrument mute tests and the corresponding
impact on C28 testing.

A preliminary package of the Command and Data System Version 9 Flight
Software was delivered to the ITL for Huygens Probe relay testing. Probe
relay testing has begun in subsystem mode with this new build of the
flight software.

The entire set of modules for Mission Sequence Subsystem (MSS) D7.6 has
been successfully tested both individually and in small groups by the ITL
and High Speed Simulator, and an integrated retest is planned for later
this week in preparation for the MSS D7.6 delivery.

The CDA Remote Terminal Interface Unit (RTIU) has been successfully
tested, and the new RTIU for RPWS is scheduled to begin testing later this
week. The RTIU converts the 1553 real-time instrument data interface to an
Ethernet interface for data processing and performance testing with the
instrument engineering model.

An on-line Risk Management Tool has been completed for Cassini. Mission
Assurance has begun the process of entering data from the Significant Risk
List, for risk tracking and assessment. Following a few additional
modifications and data entry, the tool will be rolled out for use by the
Cassini Risk Team.

A delivery review for the Advanced Multi-Mission Operations System V26.2
release was held this week. This version implements necessary capabilities
for the Gravitational Wave Experiment.

The Program Review Plan has been updated and distributed to the flight
team for review by Mission Assurance. The plan reflects the high-level
review process to assess readiness for SOI, probe relay, and Saturn tour
operations, and includes an integrated schedule of program level reviews.

The Cassini Design Team met to collect comments from Cassini personnel on
the review process for the Ground Data System and Tour Downlink Operations
Concepts reviews. These "lessons learned" comments are being collected by
System Engineering for evaluation and implementation in future reviews.

The Mission Planning team held a review of the Cassini navigation tracking
requirements. Topics included having ranging "on" at all times as a
default, reductions in the 2-way Doppler requirement, and alternative
solutions to a requirement that one third of all Cassini DSN support come
from the Madrid tracking station.

A Cassini image of Jupiter is featured in the September issue of Sky and
Telescope Magazine.


August 9, 2001

NASA SELECTS ADVANCED TECHNOLOGY CONCEPTS FOR FURTHER STUDY

NASA's New Millennium Program, managed by the Jet
Propulsion Laboratory in Pasadena, Calif., has selected 13
technology organizations to study advanced technologies that
may fly in 2004 and 2005 as part of the Space Technology 7
project.

Space Technology 7 will test and validate advanced
technologies that may become part of future NASA space
missions. The newly-contracted studies will be completed by
November. The technology concepts and providers are:

-- Aero-Entry/Capture/Maneuver -- technologies that allow a
spacecraft to be captured into orbit via sophisticated
controlled entry into atmospheres of planets (provided by the
Charles Stark Draper Laboratory, Inc., Cambridge, Mass.; NASA
Langley Research Center, Hampton, Va.; Lockheed Martin
Astronautics Operations Space Systems, Denver, Colo.)

-- Autonomy and On-board Processing -- software and hardware
for an autonomously operated mission with a rapid sense-
decide-act loop that integrates on-board science processing,
activity planning and subsystem decision conflict resolution
(provided by NASA Ames Research Center, Moffett Field, Calif.;
JPL; Massachusetts Institute of Technology, Cambridge, Mass.;
the Robotics Institute, Carnegie Mellon University,
Pittsburgh, Pa.; BAE Systems, Information and Electronics
Systems Integration Inc., Manassas, Va.)

-- Disturbance Reduction System -- sensor and thrust-producing
technologies to control a space vehicle's trajectory so that
its payload responds only to gravitational forces (provided by
Stanford University, Stanford, Calif.; Busek Co. Inc., Natick,
Mass.)

-- Solar Sail System -- technologies to deploy, control and
operate a solar sail (provided by JPL; Swales Aerospace,
Beltsville, Md.; Arizona State University, Tempe, Ariz.; AEC-
Able Engineering Company, Inc., Goleta, Calif.)

"The Space Technology 7 integrated system flight
validation concepts are very challenging advanced
technologies," said Dr. Chris Stevens, Program Manager of the
New Millennium Program at JPL. "I am very pleased by the
number and quality of the responses to the solicitation and
look forward to the results of the ST7 Concept Study Reports."
In December 2001, an independent review board at NASA
will evaluate the reports and select which technology will
fly.

Further information on the New Millennium Program is
available at
http://nmp.jpl.nasa.gov .

The New Millennium Program was created in 1994 to
identify, develop and flight-validate advanced technologies
that can lower costs and enable critical performance of
science missions in the 21st century. The program is managed
by JPL for NASA's Office of Earth Science and Office of Space
Science, Washington, D.C. JPL is a division of the California
Institute of Technology in Pasadena.


SPACECRAFT RIDING HIGH TO CATCH SOME RAYS

NASA's Genesis spacecraft launched flawlessly atop a
Delta 7326 rocket from Florida's Cape Canaveral Air Station at
12:13:40 p.m. EDT (9:13:40 a.m. PDT) today.

Genesis will become the first mission ever to return a
sample of extraterrestrial material from beyond the Moon when
it catches a piece of the Sun to return to Earth.

The Genesis team reported that the spacecraft was in
excellent health and that its power and temperature levels are
normal. The spacecraft is in communication with NASA's Deep
Space Network, and is controlled through the mission
operations area at NASA's Jet Propulsion Laboratory, Pasadena,
Calif., where the mission is managed.

At 64 minutes, 12 seconds into the mission -- or 1:17
p.m. EDT -- the Genesis spacecraft separated from the Delta's
third stage. Immediately after separation, Genesis' solar
arrays unfolded and pointed toward the Sun. The spacecraft's
signal was successfully acquired by the NASA Deep Space
Network complex at Goldstone, Calif., 85 minutes after launch
at 1:38 p.m. EST.

In September, Genesis will arrive at a point where the
gravities of the Sun and Earth are balanced. It will open its
collector arrays and begin to monitor and collect the solar
wind, ions flowing from the outer layer of the Sun. The
samples of solar wind it returns will help scientists
understand how the solar system evolved.

In September 2004, Genesis will return to Earth. The
capsule in which the samples are sealed will plummet to Earth,
slow with the aid of a parachute and be snagged in mid-air by
a helicopter. The precious samples will be airlifted to the
Johnson Space Center, Houston, Texas, where they will be
distributed for scientific analysis and safely curated in
order to be available for the next century of planetary
science studies.

JPL, a division of the California Institute of
Technology, manages the Genesis mission for NASA's Office of
Space Science, Washington, D.C. Lockheed Martin Astronautics,
Denver, Colo., designed and built the spacecraft and will
operate it jointly with JPL. Major portions of the payload
design and fabrication were carried out at the Los Alamos
National Laboratory in New Mexico and at NASA's Johnson Space
Center, Houston, Texas.

Additional information is available oline at
http://genesismission.jpl.nasa.gov and http://www.jpl.nasa.gov.


August 8, 2001

2001 News Releases

Spacecraft Riding High to Catch Some Rays
Delta II rocket in Earth orbit
Go to Genesis home page

      NASA's Genesis spacecraft launched flawlessly atop a Delta 7326 rocket from Florida's Cape Canaveral Air Station at 12:13:40 p.m. EDT (9:13:40 a.m. PDT) today.

      Genesis will become the first mission ever to return a sample of extraterrestrial material from beyond the Moon when it catches a piece of the Sun to return to Earth.

      The Genesis team reported that the spacecraft was in excellent health and that its power and temperature levels are normal. The spacecraft is in communication with NASA's Deep Space Network, and is controlled through the mission operations area at NASA's Jet Propulsion Laboratory, Pasadena, Calif., where the mission is managed.

      At 64 minutes, 12 seconds into the mission -- or 1:17 p.m. EDT -- the Genesis spacecraft separated from the Delta's third stage. Immediately after separation, Genesis' solar arrays unfolded and pointed toward the Sun. The spacecraft's signal was successfully acquired by the NASA Deep Space Network complex at Goldstone, Ca., 85 minutes after launch at 1:38 p.m. EST.

      In September, Genesis will arrive at a point where the gravities of the Sun and Earth are balanced. It will open its collector arrays and begin to monitor and collect the solar wind, ions flowing from the outer layer of the Sun. The samples of solar wind it returns will help scientists understand how the solar system evolved.

      In September 2004, Genesis will return to Earth. The capsule in which the samples are sealed will plummet to Earth, slow with the aid of a parachute and be snagged in mid-air by a helicopter. The precious samples will be airlifted to the Johnson Space Center, Houston, Texas, where they will be distributed for scientific analysis and safely curated in order to be available for the next century of planetary science studies.

      JPL, a division of the California Institute of Technology, manages the Genesis mission for NASA's Office of Space Science, Washington, D.C. Lockheed Martin Astronautics, Denver, Colo., designed and built the spacecraft and will operate it jointly with JPL. Major portions of the payload design and fabrication were carried out at the Los Alamos National Laboratory in New Mexico and at NASA's Johnson Space Center, Houston, Texas.

      Additional information is available on the Internet at: http://genesismission.jpl.nasa.gov and http://www.jpl.nasa.gov.


August 7, Mid Day News 2001

NOAA FISHERIES TO REVIEW DECLINES IN
NORTHWEST ORCA POPULATION

The National Marine Fisheries Service (NOAA fisheries), an agency of the
Commerce Department's National Oceanic and Atmospheric Administration
(NOAA), announced today that it will study the reasons behind a decline in
the number of killer whales that congregate in Washington state's Puget
Sound and Strait of Juan de Fuca in summertime.
The agency will begin a formal status review based on a conservation
coalition request to provide the whales Endangered Species Act (ESA)
protection. The review is the first in a series of steps that could lead
to ESA protection by mid-2003.

"We take very seriously the recent declines in killer whale populations
and are determined to find out what's causing it," said Donna Darm, the
acting head of NOAA fisheries' Northwest regional office in Seattle.
"Accepting this petition to conduct the review is an important first step
in determining an appropriate course of action."

NOAA fisheries said it would now convene a biological review team of
killer whale experts to try to find out if these whales constitute a
distinct population segment as defined by ESA, why the whale's population
is declining, and to make a recommendation about whether the agency should
formally propose an ESA listing next May.

The Northwest's familiar black and white killer whales, also called orcas,
are officially known as the "eastern North Pacific southern resident stock
of killer whales," to distinguish them from other killer whale groups.
They spend their summers in Washington's Puget Sound and Strait of Juan de
Fuca and the nearby Strait of Georgia in British Columbia, where they are
the frequent object of photographers and whale-watching cruises in the area.

The southern resident population has always been small, according to NOAA
biologists, but it has fluctuated widely since record keeping started in
the early 1970's, going from the low of around 70 to a peak of about 97 in
1996. The population is now estimated to be about 78 animals.

A killer whale workshop, convened by the fisheries service in early 2000
and attended by killer whale experts from Canada and the United States,
affirmed the population drop but could draw no certain conclusions for the
reason, although it cited pollution, lack of prey (especially salmon), and
even whale watching as possible causes.

"We know so little about these animals outside their summer foraging
areas," said Brent Norberg, NOAA fisheries biologist. "We don't even know
where they spend the winter or the extent of their range. That makes
determining the reason for the decline quite a challenge."

If NOAA fisheries decides to formally propose the whales for ESA
protection, it would have another year to complete more scientific work,
hold public hearings and make a final determination, likely by May 2003.
In the meantime, it will meet with scientists, including those from the
state and tribes, to familiarize them with the steps involved in an ESA
status review and to solicit information needed by the biological review team.

The petition to list the southern resident killer whales and designate
their critical habitat was submitted by a coalition of conservation groups
that included the Center for Biological Diversity, Center for Whale
Research, Whale Museum, Ocean Advocates, Washington Toxics Coalition, Orca
Conservancy, American Cetacean Society, Friends of the San Juans, People
for Puget Sound, Cascade Chapter of the Sierra Club, Project Seawolf and
Ralph Munro.

NOAA's National Marine Fisheries Service (NOAA fisheries) is dedicated to
protecting and preserving our nation's living marine resources through
scientific research, management, enforcement, and the conservation of
marine mammals and other protected marine species and their habitat.

Further information including a copy of the petition is available at
http://www.nwr.noaa.gov

To learn more about NOAA fisheries, please visit http://www.nmfs.noaa.gov


Today on Galileo
Tuesday through Thursday, August 7-9, 2001
The Conclusion of the Io 31 Encounter

The pace has truly slowed down, now, as the Flight Team heaves a sigh of
relief at the successful encounter. But there are still a few choice
science observation opportunities to take advantage of. On Tuesday, at 6:43
a.m. PDT [See Note 1], the Solid State Imaging camera (SSI) takes a 3-color
picture of the face of Io which perpetually faces Jupiter, looking for
recent volcanic activity.

Then at 7:39 a.m. PDT, SSI looks at Jupiter for over two hours, taking 13
pictures, mostly through a green filter, of an area just north of the
equator. By watching the same area of clouds over time, scientists can
measure the propagation speed of mesoscale, or medium-scale, waves in the
visible clouds. The motions of these clouds provides a probe into what is
occurring in the underlying layers of the atmosphere. The wavelength and
speed of these waves give information about the thermal stratification of
the atmosphere, and about wind shear at depth, which affect the meteorology
at the cloud-top levels.

At 10:17 a.m. PDT the instruments that measure the electromagnetic fields
and particles of the Jovian environment end their period of continuous data
collection, which began 59 hours ago, on Saturday.

At 1:50 p.m. PDT, a routine test of the on-board gyroscopes is performed.
These gyros have shown a great sensitivity to the high radiation
environment through which we fly. This test will determine if the software
scale factors that are used to interpret the signals provided to the
spacecraft's attitude control software will need to be updated prior to our
next required use of the gyros.

Wednesday morning, at 2:20 a.m. PDT, the Near Infrared Mapping Spectrometer
(NIMS) again looks at the area trailing the Great Red Spot in Jupiter's
atmosphere, looking at cloud dynamics and compositional variation in the
region.

At 3:26 a.m. PDT, SSI takes one last look at Io, a 3-color picture of the
face of the satellite which forever faces away from Jupiter. This picture
will also capture the Tvashtar volcano, arguably our most exciting target
for this flyby. This is our last recorded observation for this orbit,
because at 1:48 p.m. PDT, we begin playing back all of the data that we
have stored on the tape recorder over the last 4 days.
As we begin playing the data back, we are also using the large 70-meter
(230 foot) diameter communications antenna near Canberra in Australia to
send up the next series of commands that will govern the Galileo
spacecraft's activities for the next two months of cruise. On Friday at
2:55 p.m. PDT, the scepter of control is passed to this new set of
commands, and we bid a fond (and tired!) farewell to the Io encounter.


NASA Marshall Space Flight Center
Huntsville, Ala. 35812
For Release: Aug. 7, 2001

RELEASE: 01-264

NASA's Second Generation Reusable Launch Vehicle Program advances
propulsion technology with successful engine test series


NASA's Second Generation Reusable Launch Vehicle Program - also
known as the Space Launch Initiative - is making advances in propulsion
technology with this third and final successful engine hot-fire designed
to test electro-mechanical actuators.

Information learned from this hot-fire test series about new
electro-mechanical actuator technology - which controls the flow of
propellants in rocket engines - could provide key advancements for the
propulsion systems of future spacecraft.

The test of twin Linear Aerospike XRS-2200 engines, originally built
for the X-33 program, was performed Monday, Aug. 6, at NASA's Stennis
Space Center, Miss. The engines were fired for the planned 90-seconds and
reached a planned maximum power of 85 percent.

The test was originally slated to attain full-power during
100-seconds of testing. Prior to the test, engineers determined the
necessary results could be achieved at reduced duration and power. Based
on this determination, both planned duration and planned power were
reduced.

Two shorter hot-fires of the aerospike engines were performed last
month in preparation for the final test firing on Aug. 6.

The Second Generation Reusable Launch Vehicle Program, led by NASA's
Marshall Space Flight Center in Huntsville, Ala., is a technology
development program designed to increase safety and reliability while
reducing costs for space travel.

"Because every engine proposed by industry for a second generation
vehicle has electro-mechanical actuators, we took advantage of these
aerospike engines already on the test stand to explore this relatively new
technology now -- saving us valuable time later," said Garry Lyles,
Propulsion Projects Office manager of the Second Generation Reusable
Launch Vehicle Program at the Marshall Center. "This data is critical
toward developing the confidence required to support the use of these
actuators on future launch vehicles."


Electro-mechanical actuators electronically regulate the amount of
propellant (fuel and oxidizer) flow in the engine. The new technology is a
potential alternative and improvement to the older pneumatic and
hydraulic-fluid systems currently used by the aerospace industry to drive
and control critical rocket engine valves.

"This series of engine firings tested the actuator control system in
what we call a 'real condition of use' environment," said Dr. Donald
Chenevert, electro-mechanical actuator project manager at the Stennis
Center. "Firing allows us to see how the integrated system handles the
extreme cold of cryogenic propellants, the stress loads of the propellants
pushing through the valves, and the dynamic response to commanded flow
rate changes. Additionally, we have many other unique conditions such as
shock and vibration loads not found in a lab, so we capture more realistic
data about the true performance of the actuators."

Engineers are performing engine post-test inspections, and early
indications are that all test objectives have been met, Chenevert said.

The final data is to be fed directly into the engine systems being
considered for a second generation reusable launch vehicle, Lyles said.

"Propulsion is one of the highest and most critical technology areas
that we are exploring," said Dennis Smith, manager of the Second
Generation Reusable Launch Vehicle Program Office at the Marshall Center.
"Our goal also is to find, improve or develop technologies such as
airframes, avionics, health management systems and ground operations - all
to make getting people and payloads into space safer and cheaper."

The Rocketdyne Propulsion and Power Unit of The Boeing Company in
Canoga Park, Calif., developed the aerospike engine and supported the
engine tests at Stennis Space Center
.


RELEASE: 01-158

FIRST NASA/DREAMTIME HIGH TECH CAMERA WILL SOAR TO SPACE STATION

NASA will take a giant leap for humankind when the first
commercially provided and flight-certified high definition
television (HDTV) camera, which will provide more visual clarity of
space activities, rides aboard Space Shuttle Discovery to become a
permanent resident on the International Space Station. Discovery is
currently scheduled for launch on Aug. 9.

High tech cameras and equipment are a prime benefit of the
multimedia agreement between NASA and Dreamtime Holdings, Inc.,
Mountain View, CA. NASA partnered with Dreamtime on May 17, 2000,
to collaborate on a variety of multimedia-related services and
products.

The partnership, in response to the Commercial Space Act of 1998,
is officially termed "The NASA/Dreamtime Agreement for the
Collaboration on Multimedia" and was negotiated to maximize NASA's
existing multimedia assets and enhance the agency's television
infrastructure.

"This will be the beginning of a return on the NASA/Dreamtime
investment," said Joe Rothenberg, NASA Associate Administrator for
Space Flight. "It marks a big milestone on the road to telling the
NASA story in a new and different way."

This HDTV camera will provide high resolution images for
documentation of space activities and for enhancement of data
collected by NASA scientists, researchers and engineers conducting
experiments. Imagery will be accessible to the news media and to
the general public through the Internet and other distribution
methods.

The camera hardware includes a Sony HDW-700A HDTV camera, telephoto
lens, wide-angle lens, battery packs and tapes. The accompanying
batteries can be recharged in orbit, enabling continuous
documentation of station activities.

Although HDTV cameras have flown aboard other space shuttle
missions, the NASA/Dreamtime camera is the first to go through
flight certification for the International Space Station. This
process also makes this the first commercially certified HDTV
camera, that is, certified at no cost to the taxpayer.

"Our partner, Lockheed Martin, did an incredible job developing new
systems to certify the camera in record time," said Bill Foster,
CEO of Dreamtime. "Images from this camera have five times the
clarity of a standard digital camera. Not only will it be able to
document space from a new perspective, it also will allow our
partners to record in real time the science of space."

HDTV cameras and equipment both for on-orbit installation and use
at NASA Field Centers are among many benefits Dreamtime expects to
deliver. In addition, the partnership, through Dreamtime efforts,
will digitize a significant portion of NASA imagery and create a
multimedia database that will allow greater public access to basic
research capabilities and free downloads of low resolution versions
of those images. It also will help enhance public awareness of NASA
by developing documentaries and educational programming for
television broadcast.


Mixed Up in Space

Imagine waking up, startled by the bright flash of a cosmic ray inside
your eyes. Groggy from sleep, you wonder ... which way is up? And where
are my arms and legs!? Throw in a dash of vertigo and occasional mild
illusions, and you're beginning to sense what it can be like to live in
space -- a world where up and down have no meaning.

FULL STORY at

http://science.nasa.gov/headlines/y2001/ast07aug_1.htm?list448368


Sonja Alexander/ Adam Mahone
Headquarters, Washington, DC August 7, 2001
RELEASE: 01-159

NASA ANNOUNCES NEW AEROSPACE SAFETY ADVISORY PANEL MEMBERS

NASA has named six new members and eight new consultants
to the Aerospace Safety Advisory Panel.

The Aerospace Safety Advisory Panel (ASAP) is a senior
advisory committee reporting to NASA and the U.S. Congress.
The panel was established by Congress after the 1967 Apollo 1
spacecraft fire, which killed U.S. astronauts Gus Grissom, Ed
White and Roger Chaffee.

New members include:
* Otto Goetz, former Chief Engineer of the Space Shuttle
Main Engine (SSME) Project;
* Sid Guttierrez, former astronaut, currently Manager of the
Physical Sciences Department, Sandia National Laboratories;
* Shirley McCarty, former Principal Director of Software
Engineering at The Aerospace Corporation;
* Retired Admiral Paul Reason, former Commander in Chief,
U.S. Atlantic Fleet;
* Roger Schaufele, Professor of Aircraft Design, California
State University;
* Robert Sieck, former Director of Shuttle Processing, NASA
Kennedy Space Center.

New Consultants include:
* Dr. Wanda Austin, Senior Vice President, The Aerospace
Corporation;
* Richard Bruckman, former Director of the FA-18 Weapon
System Support Activity, China Lake;
* Dr. Ulf Goranson, former Chief Engineer at Boeing's
Structure Labs;
* Dr. Bernard Harris, former astronaut, currently Director
of The Harris Foundation;
* Dr. Nancy Leveson, Professor, Aeronautics Department,
Massachusetts Institute of Technology;
* Forrest McCartney, former Vice President for Launch
Operations, Lockheed Martin;
* Julian May, former Vice President for Technical
Operations, Delta Airlines;
* Art Zygielbaum, former Technical Lead, NASA Jet Propulsion
Laboratory.

Additional information on the Panel may be found on the
Internet at:
http://www.hq.nasa.gov/office/codeq/codeq-1.htm


August 7, 2001

KENNEDY SPACE CENTER
SHUTTLE and PAYLOAD PROCESSING STATUS_REPORT

NOTE: This is an orbiter processing report and does not necessarily reflect
the chronological order of upcoming Space Shuttle flights. Visit
http://www-pao.ksc.nasa.gov/kscpao/schedule/schedule.htm on the KSC Home
Page for the latest schedule of future Shuttle missions.

MISSION: STS-105 - 11th ISS Flight (7A.1) - Leonardo MPLM
VEHICLE: Discovery/OV-103
LOCATION: Launch Pad 39A
TARGET KSC LAUNCH DATE/TIME: August 9, 2001 at 5:38 p.m. EDT
TARGET KSC LANDING DATE/TIME: August 21, 2001 at about 1:17 p.m.
MISSION DURATION: 11 days, 19 hours and 39 minutes
CREW: Horowitz, Sturckow, Barry, Forrester; (ISS up) Culbertson, Dezhurov,
Turin; (ISS down) Usachev, Voss, Helms,
ORBITAL INSERTION ALTITUDE and INCLINATION: 122 nautical miles/51.6 degrees

Shuttle Processing Note: After a thorough engineering evaluation, Shuttle
managers today determined that the hydraulic power unit on Space Shuttle
Discovery's left-hand solid rocket booster is ready for flight with no
additional work required.

The launch countdown began on time at 5 p.m. today in firing room No. 3. and
preparation at Pad 39A continues on schedule toward the Aug. 9, STS-105
launch date. Discovery's aft compartment has been closed out for flight and
Shuttle ordnance installation is complete. Payload interface verification
testing is also complete.

The STS-105 crew and Expedition 3 crew arrived at KSC Sunday at about 1:15
p.m. to begin final preparation for flight.

Upcoming Milestones
Cryogenic loading of Discovery's onboard tanks Aug. 7
Flight crew equipment late stow Aug. 8
Rotating Service Structure moved away from Shuttle Aug. 8 (9:30 p.m.)
External tank loading Aug. 9 (8:42
a.m. - 11:42 a.m.)


JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109. TELEPHONE (818) 354-5011
http://www.jpl.nasa.gov

GALILEO MILLENNIUM MISSION STATUS

NASA's Galileo spacecraft has successfully completed a
flyby of Jupiter's moon Io, skimming about 200 kilometers (124
miles) above the surface of the highly volcanic moon at 0459
Universal Time today (9:59 p.m. Sunday, Pacific Daylight Time).

Engineers at NASA's Jet Propulsion Laboratory in Pasadena,
Calif., said that signals confirming the veteran spacecraft's
basic health were received five and a half hours after the flyby
via a Goldstone, Calif., antenna of the Deep Space Network.

As of 1700 UT (10 a.m. PDT) today, the spacecraft had
recorded about three-fourths of the scientific data that its
instruments had been programmed to collect during this swing
through the inner portion of the Jovian system. Besides
studying Io, Galileo has made observations of cloud patterns
on Jupiter.

Initial telemetry did not reveal whether or not Galileo
passed through a volcanic plume on Io. Galileo's route went
directly over a volcano named Tvashtar, which had been spouting a
tall plume of gases when last observed seven months ago. "As
expected, we don't have any sign at this point that the plume was
still active, but whether it was or not, we expect this flyby
will give us valuable new information about changes in the
Tvashtar area from recent activity," said JPL's Dr. Eilene
Theilig, Galileo project manager. The area was to be examined by
Galileo's camera and near-infrared mapping spectrometer.

Galileo's camera, which has had an intermittent electronic
problem for more than a year, appears not to have been working
during the closest part of the flyby. Engineers have narrowed the
cause of the problem to one of two electronic components probably
damaged by radiation from Jupiter's radiation belts. Nine or more
of the camera's 16 planned observations during the encounter
period were probably lost, Theilig said. Engineers are attempting
to restore the camera to functioning status in time for more-
distant observations planned for Tuesday and Wednesday.

Recorded data from the camera and Galileo's other
instruments will be transmitted to Earth over the next two
months. "We're looking forward to getting data back from the
observations to confirm that the scientific instruments worked as
planned," Theilig said.

The flyby's polar route was selected so Galileo could
collect magnetic measurements that might indicate whether Io
generates its own magnetic field, like the Earth, Jupiter, and
Jupiter's moon Ganymede. That information could give scientists a
better understanding of what goes on deep inside Io, the most
volcanically dynamic world in the solar system. The magnetometer
and other instruments for studying fields and particles appear to
have been working during the flyby.

Coming close enough to Jupiter to approach Io subjects
Galileo to intense natural radiation from Jupiter's radiation
belts, increasing the risk to the spacecraft's electronics.

"Galileo has already performed much longer than expected,
so we're pleased every time it completes another encounter
without showing new problems," Theilig said. "We're especially
satisfied to get the magnetic field measurements that were the
highest priority science objective for this flyby."

Galileo has already received more than three times the
cumulative radiation exposure it was designed to withstand and
has continued making valuable scientific observations more
than three years after its original two-year mission in orbit
around Jupiter.

Galileo will fly near Io again, over the south pole
instead of the north, on Oct. 16, 2001.

Additional information about the mission is available at
http://galileo.jpl.nasa.gov . Galileo was launched from NASA's
Space Shuttle Atlantis on Oct. 18, 1989. It began orbiting
Jupiter on Dec. 7, 1995. JPL, a division of the California
Institute of Technology in Pasadena, manages the Galileo mission
for NASA's Office of Space Science, Washington, D.C.


August 6, Mid-Day Edition

GENESIS NEXT PLANNED LAUNCH OPPORTUNITY AUG. 8

The launch of NASA's Genesis spacecraft aboard a Boeing Delta II
rocket has now been scheduled to occur at 12:13:40 p.m. EDT, Wednesday, Aug.
8.

Mission managers met with Eastern Range officials today to assess
the availability of the Aug. 8 launch day. Range officials confirmed their
ability to support the Genesis launch attempt with no impact to Space
Shuttle mission STS-105, currently slated for Aug. 9.

The Delta II launch vehicle and Genesis spacecraft are both in
excellent condition and ready to support the new launch date. The near term
Genesis launch period extends to Aug. 15. Genesis mission managers will
convene a follow-up launch readiness review Tuesday morning as part of
standard prelaunch preparations.

Genesis will be NASA's first sample return mission of this millennium, when
it captures a piece of the Sun and returns to Earth. It will travel to a
point where the Sun and Earth gravities are balanced, open its collector
arrays and capture elements in the solar wind. The samples will help
scientists learn about the beginnings of our solar system.


JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109.
http://www.jpl.nasa.gov

GALILEO MILLENNIUM MISSION STATUS
August 6, 2001

NASA's Galileo spacecraft has successfully completed a
flyby of Jupiter's moon Io, skimming about 200 kilometers (124
miles) above the surface of the highly volcanic moon at 0459
Universal Time today (9:59 p.m. Sunday, Pacific Daylight Time).

Engineers at NASA's Jet Propulsion Laboratory in Pasadena,
Calif., said that signals confirming the veteran spacecraft's
basic health were received five and a half hours after the flyby
via a Goldstone, Calif., antenna of the Deep Space Network.

As of 1700 UT (10 a.m. PDT) today, the spacecraft had
recorded about three-fourths of the scientific data that its
instruments had been programmed to collect during this swing
through the inner portion of the Jovian system. Besides
studying Io, Galileo has made observations of cloud patterns
on Jupiter.

Initial telemetry did not reveal whether or not Galileo
passed through a volcanic plume on Io. Galileo's route went
directly over a volcano named Tvashtar, which had been spouting a
tall plume of gases when last observed seven months ago. "As
expected, we don't have any sign at this point that the plume was
still active, but whether it was or not, we expect this flyby
will give us valuable new information about changes in the
Tvashtar area from recent activity," said JPL's Dr. Eilene
Theilig, Galileo project manager. The area was to be examined by
Galileo's camera and near-infrared mapping spectrometer.

Galileo's camera, which has had an intermittent electronic
problem for more than a year, appears not to have been working
during the closest part of the flyby. Engineers have narrowed the
cause of the problem to one of two electronic components probably
damaged by radiation from Jupiter's radiation belts. Nine or more
of the camera's 16 planned observations during the encounter
period were probably lost, Theilig said. Engineers are attempting
to restore the camera to functioning status in time for more-
distant observations planned for Tuesday and Wednesday.

Recorded data from the camera and Galileo's other
instruments will be transmitted to Earth over the next two
months. "We're looking forward to getting data back from the
observations to confirm that the scientific instruments worked as
planned," Theilig said.

The flyby's polar route was selected so Galileo could
collect magnetic measurements that might indicate whether Io
generates its own magnetic field, like the Earth, Jupiter, and
Jupiter's moon Ganymede. That information could give scientists a
better understanding of what goes on deep inside Io, the most
volcanically dynamic world in the solar system. The magnetometer
and other instruments for studying fields and particles appear to
have been working during the flyby.

Coming close enough to Jupiter to approach Io subjects
Galileo to intense natural radiation from Jupiter's radiation
belts, increasing the risk to the spacecraft's electronics.

"Galileo has already performed much longer than expected,
so we're pleased every time it completes another encounter
without showing new problems," Theilig said. "We're especially
satisfied to get the magnetic field measurements that were the
highest priority science objective for this flyby."

Galileo has already received more than three times the
cumulative radiation exposure it was designed to withstand and
has continued making valuable scientific observations more
than three years after its original two-year mission in orbit
around Jupiter.

Galileo will fly near Io again, over the south pole
instead of the north, on Oct. 16, 2001.

Additional information about the mission is available at
http://galileo.jpl.nasa.gov . Galileo was launched from NASA's
Space Shuttle Atlantis on Oct. 18, 1989. It began orbiting
Jupiter on Dec. 7, 1995. JPL, a division of the California
Institute of Technology in Pasadena, manages the Galileo mission
for NASA's Office of Space Science, Washington, D.C.


Michael Braukus
Headquarters, Washington

RELEASE: 01-156

NASA SELECTS TWO DESIGN TOOLS AS SOFTWARE OF THE YEAR

Computer programs that reduce aircraft engine analysis
time and improve the study of fluid dynamics in rocket
engines have been selected as NASA's 2001 software of the
year winners.

The Numerical Propulsion System Simulation (NPSS) software
allows multi-fidelity analysis in designing aircraft engines,
offering key technological advances to increasing the U.S.
aerospace industry's competitiveness. The General Electric
Aircraft Engines Co. estimates a 55 percent reduction in
engine analysis time using this new software.

The development of NPSS was led by Cynthia Gutierrez Naiman
of NASA's Glenn Research Center, Cleveland, and included a
team of 39 other engineers from Glenn; Arnold Engineering
Development, Arnold Air Force Base, TN; Dynacs, Cleveland;
General Electric Aircraft Engines Co., Cincinnati; GESS,
Cleveland; Honeywell, Tucson, AZ; Pratt & Whitney, East
Hartford, CT; Modern Technologies Corp., Middleburg Hts., OH;
Rolls Royce Corp., Indianapolis; RS Information Systems,
Inc., Cleveland; and The Boeing Company, Seattle.

The Generalized Fluid System Simulation Program (GFSSP) is a
general purpose computer program for analyzing fluid-flow
rate, pressure, temperature and concentration in rocket
engines, turbo pumps and fuel tanks. The program is capable
of modeling liquid fuel phase changes including
compressibility, mixture thermodynamics and the effects of
external influences, such as gravity and centrifugal force.

The development of the GFSSP software eliminates the need to
develop specific-purpose software. Cost savings also can be
realized through reducing hardware testing and continuous
improvement. It is estimated that one organization's use of
GFSSP can save between $825,000 and $1.5 million.

Alok Kumar Majumdar of NASA's Marshall Space Flight Center,
Huntsville, AL, led the development team, which included
engineers from Marshall, ERC, Inc. and Sverdrup Technology,
also of Huntsville.


Kyle Herring
Johnson Space Center, Houston, TX
RELEASE: 01-157

ASTRONAUT CABANA ASSUMES NASA LEAD OPERATIONS ROLE IN RUSSIA

Astronaut Robert D. Cabana has been named NASA's
Director, Human Space Flight Programs, Russia, effective Aug.
8. He assumes this role at a time when the International
Space Station (ISS), while still under construction, has
become self-reliant, and larger and more capable than any
other space station in history.

Cabana will act as Deputy to both the ISS Program Manager and
the Director of the Johnson Space Center, Houston, with full
authority to represent both in all matters pertaining to NASA
human space flight activities in Russia.

Cabana replaces astronaut Michael A. Baker (Capt., USN) who
has served as head of the Moscow operation since its
inception in January 1998. At that time, the office was
formed to facilitate the transition from the Phase One
Shuttle-Mir program to the assembly and operation of the
International Space Station.

"Mike has done an outstanding job in coordinating NASA's
operational efforts in Russia and provided leadership and
friendship to both the NASA team in Moscow and our Russian
colleagues," said Roy Estess, Acting Director of the Johnson
Space Center. "We look forward to having him back in
Houston."

As Director, Human Space Flight Programs, Russia, Cabana will
be NASA's lead representative to the Russian Aviation and
Space Agency (Rosaviakosmos) and its contractors. His role is
to continue oversight of all human space flight operations,
logistics, and technical functions, including NASA's mission
operations in Korolev and crew training at the Gagarin
Cosmonaut Training Center in Star City .

"I can think of no one better suited to continue the role
established by Mike Baker as the International Space Station
moved from dreams to reality," said Estess. "The station has
reached another milestone with the delivery of the Airlock
Quest, and we are fortunate to have Bob lend his leadership
and space flight expertise to the program as it continues to
grow."

Currently, Canadian Space Agency astronaut Chris Hadfield
(Col., CAF) is serving as the Director of Operations, Russia,
overseeing training activities for astronauts in Star City.

"Bob's leadership skills and experience provide an excellent
backbone for NASA's partnership with our Russian colleagues,"
said Tommy Holloway, ISS Program Manager. "He has been a
great asset to the program as an interface with not only our
Russian colleagues, but with all the ISS International
Partners, and I am confident he will continue to do so,
albeit from another location."

Cabana has flown four shuttle missions, including the first
assembly flight of the International Space Station, when
Endeavour delivered the Unity module and joined it to the
Zarya Control Module, the first component of the station
launched into orbit. Unity now serves as the attachment point
for both the U.S. Laboratory Destiny and the newest U.S.
element the Airlock Quest, as well as a shuttle docking port.
Cabana's management roles have included Chief of the
Astronaut Office for three years during the Shuttle-Mir
Program and most recently Manager for International
Operations for the ISS Program.

Baker has flown four shuttle missions, including serving as
commander of Atlantis' STS-81 mission in January 1997, the
fifth docking of a shuttle to the Mir Space Station. Prior to
that flight, Baker served as the NASA Director of Operations
at Star City from March to October 1995.

For additional information on Cabana, Baker, Hadfield or any
astronaut, visit the NASA Internet biography home page at:
http://www.jsc.nasa.gov/Bios/

For more information on the International Space Station and
Space Shuttle Programs, tour the NASA human space flight web
site at:
http://www.station.nasa.gov


NOAA to Participate in Tsunami Review, International Symposium

Significant advances in efforts to protect coastal residents from
tsunamis, the large and potentially deadly waves usually generated by
seismic events in the ocean, have resulted from a team effort led by the
Commerce Department's National Oceanic and Atmospheric Administration
(NOAA). The accomplishments and the next steps will be the subjects of a
review of the Tsunami Hazard Mitigation Program and an international
symposium during the week of August 6 in Seattle, Wash.
"It's time for us to take a look at what we've accomplished since we first
developed a coordinated plan to save lives and property five years ago.
But more important, we have a chance to use new science and technology to
improve the tsunami mitigation plan for the next five," said Eddie N.
Bernard, director of NOAA's Pacific Marine Environmental Laboratory in
Seattle and chair of the tsunami project steering group.

The tsunami program is a federal/state effort to seek ways of warning
residents in coastal areas of the hazard, as well as try to mitigate the
damage from such events. The program began in 1996. Program
accomplishments include:

§ Forming a successful partnership between the five Pacific states
(Hawaii, California, Oregon, Washington and Alaska).
§ Establishing consistent tsunami mitigation plans, evacuation route signs
and procedures for communities in the five states.
§ Developing tsunami inundation maps that show areas that could be
affected by tsunami waves. These maps have led to the creation of
mitigation plans and evacuation routes for communities.
§ Upgrading NOAA's tsunami warning system to significantly reduce warning
times and increase the ability to detect tsunamis started by earthquakes
and accurately track tsunamis across the ocean.

NOAA's ability to upgrade its warning and tracking systems and the states'
ability to develop mitigation plans and evacuation procedures has led to a
process where individual towns and cities can take it one step further to
become certified and recognized as a community that is TsunamiReady,"
Bernard said.

On June 30, Ocean Shores, Wash., was recognized as the first community to
earn TsunamiReady designation.

The review panel will take a look at the accomplishments of the federal
and state partnership and discuss the next steps in tsunami warning and
awareness activities and regional coordination.

The symposium will feature an international array of scientists and
engineers who specialize in tsunami research and mitigation. Presentations
will focus on tsunami-related technical advances and the state of the
science. Topics include tsunami generation, prediction and simulations,
disasters and mitigation, instrumentation and observations, warning and
preparedness, databases, and propagation. Among the presentations will be
an update from a tsunami response team sent to Peru to investigate the
near-shore tsunamis generated by the June 28 earthquake.

The week's events include the program review on August 7 and the
international symposium August 8-9 at the University of Washington in
Seattle. The week will conclude with a field trip on August 10 to the site
of the 1700 Cascadia earthquake and tsunami followed by a public forum in
Ocean Shores, Wash., with area officials and tsunami experts.

The Commerce Department's National Oceanic and Atmospheric Administration
(NOAA) is dedicated to enhancing economic security and national safety
through the prediction and research of weather and climate-related events
and providing stewardship of our nation's coastal and marine resources. To
learn more about NOAA, please visit http://www.noaa.gov

Agendas for the Review and the Symposium can be found at:
http://www.pmel.noaa.gov/its2001/.

For information about the Tsunami Hazard Mitigation Program, visit:
http://www.pmel.noaa.gov/tsunami_hazard/.

To learn more about the Pacific Marine Environmental Laboratory, visit:
http://www.pmel.noaa.gov.


Kennedy Space Center
KSC Release No. 98-01

GENESIS NEXT PLANNED LAUNCH OPPORTUNITY AUG. 8

The launch of NASA's Genesis spacecraft aboard a Boeing Delta II
rocket has now been scheduled to occur at 12:13:40 p.m. EDT,
Wednesday, Aug. 8.

Mission managers met with Eastern Range officials today to assess
the availability of the Aug. 8 launch day. Range officials
confirmed their ability to support the Genesis launch attempt with
no impact to Space Shuttle mission STS-105, currently slated for
Aug. 9.

The Delta II launch vehicle and Genesis spacecraft are both in
excellent condition and ready to support the new launch date. The
near term Genesis launch period extends to Aug. 15. Genesis mission
managers will convene a follow-up launch readiness review Tuesday
morning as part of standard prelaunch preparations.

Genesis will be NASA's first sample return mission of this
millennium, when it captures a piece of the Sun and returns to
Earth. It will travel to a point where the Sun and Earth gravities
are balanced, open its collector arrays and capture elements in the
solar wind. The samples will help scientists learn about the
beginnings of our solar system.


>August 6, 2001

Today on Galileo
Monday, August 6, 2001
Day 3 of the Io 31 Encounter

The day begins with our focus still firmly on Io, with Galileo only a
little over an hour past closest approach, and the view is now of a nearly
fully sunlit hemisphere of the volcanic satellite. The Near Infrared
Mapping Spectrometer (NIMS) starts today's observations at 12:08 a.m. PDT
[See Note 1] with a view of the Amirani and Maui region, looking at the
temperatures of a hot spot at Amirani and surveying the distribution of
sulfur dioxide in the area.

The Solid State Imaging camera (SSI) then follows at 12:25 with a
medium-resolution look at Masubi Fluctus (or flow). This is our first view
of this area at this resolution (393 meters per pixel or 1270 feet per
pixel). The five images taken here also capture the site of a new hot spot
first seen by NIMS during our previous encounter in May.

The ball is still in the SSI court, as it next views two other regions of
flow -- Lei-Zi Fluctus and Kanehekili Fluctus. During the approximately
three minutes that these pictures are being taken, Galileo is moving
further away from Io at 7.1 kilometers per second (4.4 miles per second).
As the distance increases, our resolution drops, and by the end of these
observations, we can only see objects 410 meters across (1330 feet).
Finally, the camera views the terminator, or day-night boundary of Io,
looking at three areas, called Surya, Tohil, and Culann. By viewing areas
near sunrise (or sunset) it is possible to use any shadows cast by the
features to determine their relative heights.

NIMS again comes to the fore, and spends the next hour constructing
temperature maps of several regions on the satellite, including the
Prometheus volcano and Emakong. These maps can be compared with data
obtained during previous orbits, such as our most recent Io flyby in
February 2000. The comparison will show if any changes have taken place in
the distribution of material, and will show if any new active regions have
cropped up.

Next, SSI views the tiny inner satellite Amalthea, with the highest
resolution we have yet achieved on this side of the body. However, given
our distance from Amalthea at the time (635,000 kilometers or 395,000
miles), this still limits us to only being able to see features larger than
6.5 kilometers (4 miles). This picture will also be used to help pin down
the exact location of Amalthea, using a technique called optical
navigation. By improving our knowledge of the orbit of this satellite, we
also improve our ability to maneuver the spacecraft to a planned close
flyby in November of next year. At that time, we will be viewing the same
side of the satellite that this view shows.

The Photopolarimeter Radiometer (PPR) instrument now rejoins the observing
armada, as it spends the next two hours mapping the entire visible surface
of Io for the first time in daylight. By comparing daytime temperatures of
features with nighttime temperatures obtained in earlier observations,
scientists will be able to determine the total amount of volcanic heat
flowing out of Io, and thus better understand the processes by which
Jupiter's tides heat Io and cause the volcanic activity. PPR then continues
with a second, half-hour map of the entire disk of Io, this time measuring
the polarization of the light, rather than the temperatures. This data
provides insight into the detailed physical structure of the surface materials.

By now, it's 7:18 a.m. PDT, and time for another quick picture of Amalthea,
to help triangulate its position. In the four and a half hours since the
previous look, both the spacecraft and the satellite, which only takes
about 10 hours to completely circle Jupiter, have moved considerably.

At 8:00 a.m. PDT PPR directs its focus on Callisto for its second of three
brief studies of the polarization of light from that satellite during this
orbit. The final observation comes at 7:37 p.m. PDT this evening.

There are longer pauses between the observations now, and it isn't until
10:00 a.m. PDT that NIMS looks again at Jupiter's atmosphere, measuring the
cloud dynamics and compositional variations in the turbulent area lying
just behind the Great Red Spot.

At 1:16 p.m. PDT, Galileo reaches this orbit's closest point to the icy
satellite Europa, which was the focus of our observations throughout most
of 1998. Our distance this time is 609,000 kilometers (380,000 miles), and,
as with Sunday's distant pass by Ganymede, Europa is too far away to
warrant any science observations.

Between 6 and 8 p.m. PDT, the Energetic Particle Detector (EPD) reloads its
memory. In the past, this instrument has shown susceptibility to the
radiation seen near Jupiter, which causes the microprocessor controlling
the instrument to stop operating correctly. Though such an upset is
certainly not guaranteed, this pre-emptive reload will restore the
instrument to a proper operating state without needing the ground
controllers to intervene.

By 9:20 p.m. PDT, the spacecraft has receded sufficiently from the fierce
radiation field of Jupiter to allow the attitude control software to look
once again for four stars to guide our way. For the past two days, we have
been relying on a single bright star, whose signal in the star tracker
sensor rises above the noise caused by the radiation. That noise has now
subsided, and fainter stars can also be reliably viewed. More stars provide
the software greater accuracy in determining the orientation of the spacecraft.

During this entire day, the suite of instruments which measure the fields
and particles in the Jupiter system have been actively, quietly, and
continuously collecting data and storing the results in the large science
data memory buffer in the spacecraft computer. These data are then relayed
to Earth whenever a ground tracking antenna views the spacecraft. The
continuity of this data is important in understanding the detailed
structure of the Jupiter environment as Galileo slices deeply into, and
then back out of, the dynamic magnetosphere of the giant planet.

-----
Note 1. Pacific Daylight Time (PDT) is 7 hours behind Greenwich Mean Time
(GMT). The time when an event occurs at the spacecraft is known as
Spacecraft Event Time (SCET). The time at which radio signals reach Earth
indicating that an event has occurred is known as Earth Received Time
(ERT). Currently, it takes Galileo's radio signals 49 minutes to travel
between the spacecraft and Earth. All times quoted above are in Earth
Received Time.

For more information on the Galileo spacecraft and its mission to Jupiter,
please visit the Galileo home page at one of the following URL's:

http://galileo.jpl.nasa.gov
http://www.jpl.nasa.gov/galileo

August 5,2001

Cassini Weekly Significant Events
for 07/26/01 - 08/01/01

The most recent spacecraft telemetry was acquired from the Goldstone
tracking station on Monday, July 30. The Cassini spacecraft is in an
excellent state of health and is operating normally. Information on the
spacecraft's position and speed can be viewed on the "Present Position"
web page, http://www.jpl.nasa.gov/cassini/english/where/ .

Recent spacecraft activities include two Radio and Plasma Wave Science
High Frequency Receiver calibrations and two Cassini Plasma Spectrometer
data set collections. The Composite Infrared Spectrometer was powered on
for instrument muting tests, and the second of the three muting tests was
completed this week. These tests are being conducted by the Spacecraft
Operations Office (SCO) in support of future Huygens Probe checkouts. The
SCO also completed an Attitude Control Subsystem Reaction Control
Subsystem calibration.

The Critical Design Review (CDR) for the Cassini Ground Data System (GDS)
was held, which included a system-level design overview from each office
and updates of the Cassini software inventory, subsystem interfaces, and
data flow.

In support of the C28 sequence development, the preliminary Sequence
Integration & Validation Package was created and released.

The C29 Science Planning Virtual Team (SPVT) Project Briefing was held,
with the Project approving the integrated plan for implementation. The
first product input port for this process falls within the next week, and
the entire C29 SPVT phase will be complete in early September.

Meetings of both the Magnetosphere and Cross-Discipline Target Working
Teams were held last week. Discussion included data input to the Cassini
Information Management System as well as MAPS campaigns and Saturn imaging
movies.

The last updates of the D27 Multi Mission Image Processing Laboratory
software were delivered for testing. These updates are evolutionary
updates to both Uplink and Downlink support software.


Today on Galileo
Sunday, August 5, 2001
Day 2 of the Io 31 Encounter

Today is a busy day, which will end with our close flyby of Io. First up,
however, at 1 a.m. PDT (see Note 1), is a measurement by the
Photopolarimeter Radiometer instrument (PPR) of a white oval storm in
Jupiter's atmosphere at around 30 degrees south latitude. These persistent
storm features have been a frequent target for Galileo's scrutiny over the
past five years, and this long-term study has yielded significant insight
into their dynamics and life-cycle. This large, counter-clockwise rotating
feature, called "BA", is about the size of the Earth. Our expectations are
that the feature, which is the product of a merger of three smaller white
ovals early in 2000, will either decay and dissipate or possibly grow
larger, similar to the Great Red Spot.

Following this, PPR turns its gaze on the north polar region of the giant
planet, an area crowded with many small storms which have a surprisingly
long life. We are observing a phenomenon first noted in ground-based
observations of Jupiter's temperatures near its arctic pole. The polar
region has an irregular boundary that appears to form a wave. Our
observations will tell us whether we can observe this phenomenon at higher
spatial resolution to refine our plans in the next orbit's encounter (in
October) to map the phenomenon at all longitudes. The Cassini spacecraft,
which passed Jupiter in December of last year, was able to make a far more
comprehensive study of a snapshot in time of the global atmospheric
environment than is possible from Galileo, with its limited data rate.
However, Galileo, being much closer to Jupiter, and for a far longer time,
can study specific features in much greater detail, and track their
evolution. Combining these two types of data is what keeps planetary
scientists happy, and provides significant advances to our knowledge of the
weather patterns on Jupiter.

At 4:30 a.m. PDT the tape is moved halfway down its length and back again.
Keeping the tape moving in this way helps prevent it from sticking to the
heads. The tape did stick in October of 1995 as Galileo first approached
Jupiter. This caused the project to change the mission strategy for the
December 1995 Jupiter Orbit Insertion period to guarantee capturing the
unique data provided by the Galileo Probe as it entered the Jupiter
atmosphere. This change in strategy meant forgoing recording any data from
the optical instruments during the 1995 Io flyby. Fields and particles data
was recorded, since that strategy was much simpler, and resulted in less
risk to the tape recorder. That unfortunate situation has meant that the Io
passes we have made in the extended mission have been that much more
exciting, due to the long wait for the data.

At 10:22 a.m. PDT Galileo reaches its closest point to the satellite
Ganymede. At 1,066,747 kilometers, however, it is too distant to provide
useful enough science return to trade the resources against the detailed
look at Io yet to come. In fact, for the remainder of the mission Ganymede
is too distant to provide a suitable target for observations, and so we have
looked our last upon this satellite!

At 2:50 p.m. PDT the spacecraft passes into the shadow cast by Jupiter. This
solar occultation lasts until 5:00 p.m. In addition, at 3:56 p.m. Galileo
also passes behind Jupiter as seen from Earth. This situation is used by the
Radio Science team. Sixteen minutes before the start of the occultation, the
radio signal sent by the spacecraft is changed to a pure tone, with no
telemetry modulation. By following carefully the changes to this signal as
it passes deeper into the atmosphere, the team can determine temperatures
and pressures of the different layers of gases and clouds. The physical
occultation lasts until 5:58 p.m., and the radio signal is changed back to
the normal telemetry mode 17 minutes later.

Evening is now upon us, and at last we turn our gaze to the primary target
for this orbit, the satellite Io. PPR once again takes the lead with a
series of observations between 6:05 p.m and 10:23 p.m. PDT. During this
time, the instrument takes a global temperature map of the satellite, and
nightside detailed temperature maps of the Pele and Loki volcanoes. PPR also
examines the north polar region of the satellite, which was found to be
unexpectedly warm during previous flybys. A scan from the equator to the
south pole will pass over the Pillan volcano. Finally, a map of the Lei Kung
Fluctus region is performed. Fluctus is Latin for 'flow', and indicates that
this area seems to be a large lava flow.

One additional unique aspect to this flyby is that this is the first time in
the nearly six years of the Galileo orbital mission that the spacecraft has
had a major encounter activity with no ground communications coverage. The
large, 70-meter diameter antenna near Madrid, Spain is currently undergoing
an extensive series of equipment modifications to provide support for future
space missions, and is unable to view Galileo during this encounter. At the
two other Deep Space Network communications complexes that are used to track
spacecraft, Galileo sets below the horizon as seen from the Canberra,
Australia site about 3 hours before closest approach, and does not rise as
seen from the Goldstone, California site until 5 hours after closest
approach. During this time, all data acquired on the spacecraft are stored
either on the tape recorder or in buffer areas of computer memory.

At 10:14 p.m. PDT, the spacecraft is only a half hour away from Io, and the
Fields and Particles instruments begin to record their data continuously at
a high rate (at least 7.68 kilobits per second, far higher than the possible
real-time rates of 20 to 60 bits per second) for the next hour.

At 10:19 p.m. PDT, the Energetic Particle Detector (EPD) instrument cycles
its power and reloads its memory to prepare for the close Io flyby. In the
event that the high radiation environment near Io and Jupiter causes the
instrument electronics to hiccup, this reset should provide the best
protection for the most critical data collection at closest approach.

Activities start coming thick and fast now, as we get closer. At 10:26 p.m.
PDT the Near Infrared Mapping Spectrometer (NIMS) joins the fray, observing
the Pele, Pillan, and Isum regions on the night side of Io, looking for
thermal anomalies and measuring any volcanic activity. While these
observations are taking place, the Solid State Imaging camera (SSI) is
cycling its power in preparation for the highest resolution images to come.

At 10:41 p.m. PDT, the spacecraft reaches its closest approach to Jupiter,
at a distance of 4.9 Jupiter radii (350,300 kilometers or 217,720 miles)
above the cloud tops. This is not the closest we've been to the planet. That
distinction came during our December 1995 entry into Jupiter orbit, when we
passed by at 3.0 Jupiter radii (214,500 kilometers or 133,300 miles).

Once again, PPR steps to the fore, and at 10:43 p.m. PDT directs its gaze
straight down towards the satellite. At this time, the spacecraft pointing
is fixed, and it is Io that passes before our view, as Galileo flies by at
7.1 kilometers per second (4.4 miles per second or 15,840 miles per hour!).
Our closest point to Io comes at 10:48 p.m. PDT, when Galileo is a scant 200
kilometers (124 miles) over the surface. Since we are flying over high
northern latitudes, just 13 degrees from the pole, PPR will be able to study
in great detail the unusually high temperatures seen in this region.

Two minutes later, at 10:50 p.m. PDT, SSI captures a series of six pictures
of Io in less than two minutes, looking at the volcano Tvashtar. In these
pictures, we will be able to see features as small as 3.4 meters across (11
feet). The Tvashtar volcano was active when Galileo and Cassini viewed the
area in December of 2000. The Galileo camera spied a bright lake of lava at
the site, and the Cassini camera, using an ultraviolet filter, was able to
detect a plume of erupting gaseous material reaching nearly 400 kilometers
(250 miles) above the surface. There is no direct evidence that the site is
still active at this time, but if there is any volcanic activity as we fly
by, either lava flows or eruptions, Galileo will acquire its closest look
yet at active volcanism on Io, the most geologically active body in the
solar system.

In comparison, the MISR instrument aboard NASA's Terra satellite has
recently been observing the active eruption of Mt. Etna on the island of
Sicily in the Mediterranean Sea. Amusingly, from a linguistic standpoint,
the plume of ash and dust from Mt. Etna is now drifting across the Ionian
Sea! Is this a portent for Galileo's view? The oracles have been mute on
this point. The Terra satellite flies at an altitude of 705 kilometers (440
miles) above the Earth, whereas Galileo's closest point to Tvashtar is only
320 kilometers (200 miles). For pictures of Mt. Etna from the Terra
spacecraft, visit the web site http://www-misr.jpl.nasa.gov/ , and then
imagine what Galileo might be seeing from less than half that distance!

As SSI catches its breath from these pictures, NIMS takes over and maps the
distribution of sulfur dioxide (SO2) in the high northern latitudes of Io,
starting at 10:52 p.m. PDT. Then at 10:59 p.m. SSI sets its sights on the
volcano Prometheus, as this feature sits on the limb of Io as seen from the
spacecraft. When viewed in this way, any possible volcanic eruptions can be
seen silhouetted against the dark of the sky. Two minutes later, SSI
returns to gaze at Tvashtar from greater range for another six pictures.
These more distant, wider angle views of the area provide more general
context information, with a resolution of about 52 meters (170 feet),
within which the earlier pictures will give us the fine detail.

For ten minutes starting at 11:04 p.m. PDT, NIMS will be mapping the
Tvashtar region, and the instrument's spectral measurements will provide
information about the composition of the surface materials.

At 11:21 p.m. PDT, SSI begins a series of images of various interesting
locations on Io, with exotic names like Savitr, Amirani, Maui, and Itzamna
Patera. These names, as are all the feature names on Io, have been chosen
by the International Astronomical Union to represent volcanic beings from
myth and history from many Earthly cultures.

At 11:28 p.m. PDT, NIMS begins a 16-minute observation of the Gish Bar hot
spot, looking for changes that may have occurred since we last viewed this
feature. Volcanic regions on Io are extremely variable, and a particular
site may be active on one orbit, then dormant on the next only a month
later.

PPR, which started the observation set today, neatly frames this 24-hour
period with a final observation, a single scan from the north pole to the
south pole on Io, measuring the temperatures and helping to study the
unusual polar warming on this bizarre satellite.

At this point in the flyby, we have still used up only half of the tape in
our on-board tape recorder. Once past closest approach to Io, Galileo is
able to look back and see a nearly fully sunlit hemisphere, which sets the
stage for a whole new set of observations being possible. But that is a
story for another day. Tomorrow...


http://www.jpl.nasa.gov/solar_system/features/lopes_index.html

Spotlight:
Lava Flows Freely on Jupiter's Moon Io

From Interview-August 1, 2001

Dr. Rosaly Lopes is on the team for one of the Galileo instruments that has
returned information about active volcanoes, the near-infrared mapping
spectrometer, or NIMS.

Scientists using NASA's Galileo spacecraft have made many discoveries about
the volcanoes on Jupiter's moon Io since Galileo began orbiting Jupiter in
1995. The spacecraft's final three encounters with Io are in August and
October, 2001, and January 2002.

Dr. Rosaly Lopes, a volcanologist at the Jet Propulsion Laboratory, is on
the science team for one of the Galileo instruments that has returned
information about active volcanoes, the near-infrared mapping spectrometer,
or NIMS. She is a native of Brazil who earned her doctorate from the
University of London. In September 1979, she was doing field research at Mt.
Etna, on the Italian island of Sicily, when a crater only about a mile away
from her exploded and killed several people. "I really learned to respect
volcanoes," Lopes said.

Q: How did you get interested in studying volcanoes on Io?
A: I studied volcanoes on Earth and Mars for my Ph.D. I had just started in
1979, the year Voyager discovered volcanoes on Io, so that was a great
excitement. My opportunity to study volcanoes on Io came with Galileo, when
I started planning the Io observations for NIMS.

Q: How volcanic is Io?
A: We consider Io the most volcanic body in the solar system because its
volcanoes put out the most heat. We have found more than 100 volcanoes on
Io, but Earth has more than 600 active volcanoes, so it's not the number
that make Io the most volcanic. It's the heat output. Io is only about
one-third as big as Earth, but it puts out about twice the energy. One of
Io's volcanoes, Loki, is more powerful than all of Earth's volcanoes
combined.

Q: Are Io's volcanoes like Earth's volcanoes?
A: Yes and no. The types of eruptions we have observed on Io are similar to
types of eruptions on Earth -- lava flows, calderas, fire fountains like in
Hawaii -- but there are some very different aspects. One is that lava on Io
is much hotter than any lava that flows on Earth today. Billions of years
ago Earth had lava that hot. Another difference is that the calderas, the
volcanic craters, on Io are much larger than on Earth. Lava flows are much
larger, too. [An Io volcano named] Amirani has a lava flow 300 kilometers
[190 miles] long, and that's much longer than any on Earth. Globally, Io
erupts more than 100 times as much lava per year as Earth, including Earth's
undersea eruptions.

Q: Where could you go on Earth that might look like Io?
A: The big island of Hawaii has the Kilauea volcano that has been active for
about two decades. Yellowstone is a large caldera that has many areas with
brightly colored sulfur. Stromboli [in Italy] has been active for at least
2,000 years. Some very old lava flows on Earth, such as some in South
Africa, are a composition called komatiite, which we think is the
composition of Io's lavas. Probably the most similar place on Earth just in
terms of the great amount of volcanic activity is under the ocean at the
mid-ocean ridge.

Q: What makes Io so volcanic?
A: Although both Earth and Io have active volcanism, the way the volcanism
happens is quite different. On Earth, volcanism is tied to plate tectonics,
and we don't believe Io has plate tectonics. Io is in a tug of war between
Jupiter and Europa and Ganymede, two of the other large moons of Jupiter,
and that is what heats it up. If Io weren't in its very peculiar orbit
around Jupiter, it wouldn't have active volcanism. It would have cooled off
a long time ago.

Q: Some people say Io looks like a pizza. What are all those bright colors?
A: We think the bright colors are due to sulfur in various forms but that
the very dark colors are due to active lavas. Every place we see high
temperatures, if we look at the surface we see dark materials. That would be
the olives on the pizza. The reds are deposits from the plumes of volcanoes.
With time, the reds become yellow because of changing to a different form of
sulfur. We're still quite puzzled by what some of the very small green areas
are. We joke and call them golf courses. They may be areas rich in sulfur
but contaminated by another material. Another possibility is they are very
olivine- rich lava. Olivine is a green mineral.

Q: What is there about Io that is still a mystery to you?
A: We still don't know if Io has its own magnetic field, like the Earth
does. That would help us understand the interior. We hope we will still get
an answer from Galileo about that. There are other questions that will still
remain after Galileo. What is the composition of the lavas? We are using
their temperature to say what is the most likely composition based on
comparison with lavas on Earth, but we don't really know whether lavas on Io
are something entirely different. We won't know that until we can go back
with more refined instruments or maybe someday go there and bring back some
samples. When we study volcanoes on Earth, one of the first things we do is
collect samples of lava and take them back to the lab, but for Io, that's a
long way in the future.
August 4, 2001

Today on Galileo
Saturday, August 4, 2001
The Encounter Begins

This morning at 4:49 a.m. PDT [See Note 1] Galileo's 31st encounter begins.
Once again, this hardy spacecraft plunges deeply into Jupiter's intense
radiation field to fly by the fascinating moon Io, the innermost of the
giant planet's four largest satellites. These four satellites, also called
the Galilean satellites, share the namesake of the spacecraft, Galileo
Galilei. This Italian astronomer spied these fascinating worlds in 1610
when he first gazed through his primitive telescope. How different things
are today, when we can visit them with robotic spacecraft such as our
Galileo, and unravel their secrets by getting up close and personal! From
tiny points of light, the Voyager and Galileo spacecraft have transformed
these bodies into full and complex worlds.

First up, at 9 a.m. PDT, the Photopolarimeter Radiometer instrument turns
on its power and performs a calibration by looking at a target plate
mounted on the spacecraft. This observation establishes a baseline reading
for the operation of the instrument against which the science measurements
taken later in the sequence can be compared. When this is completed, the
instrument sets its sights on Callisto for a measurement of the
polarization of the light from that body. By studying how the polarization
of the reflected sunlight changes as we view the body from different
angles, scientists can determine the small-scale structure of the surface.
This observation takes place near the closest approach to Callisto by
Galileo on this orbit, but that is still from a distance of 350,000
kilometers (220,000 miles), nearly three times the distance at which
Voyager 1 passed the satellite in 1979.

At 1:10 p.m. PDT, the attitude control software on the spacecraft is
configured to use a single star as its primary reference. Ordinarily, the
software uses the signals from three or four stars to accurately determine
the orientation of the spacecraft. When in the high radiation environment
close to Jupiter, however, noise floods the star scanner detector and masks
the signals from the fainter stars. By focusing on a single bright star,
whose signal is above the noise, the software can safely maintain its
knowledge of Galileo's attitude. The star being used is the same one we
used on the last flyby in May, Achernar, or Alpha Eridani, the brightest
star in the constellation of Eridanus, the River.

At 4:30 p.m. PDT, the Solid State Imaging camera (SSI) is turned off and
then turned on again, just before its first observation. In recent orbits,
the SSI instrument has experienced problems during our passage through the
radiation belts which result in completely saturated, overexposed images.
Experience has shown that cycling the power may help to clear this
situation, at least temporarily. Eight times during this encounter the SSI
instrument will cycle power and reload its internal software just before
key blocks of observations, to make sure that the instrument is as healthy
as we can make it. This first SSI observation is an attempt to view a plume
of material which may still be erupting from the Tvashtar volcano on Io.
This volcano has been extremely active lately, and is a prime target of
observations during this flyby, since the path of the spacecraft will take
it very nearly directly overhead of the feature just after closest
approach. This observation will also serve as part of a survey to determine
what other volcanic features may be currently active.

At 9:30 p.m. PDT, SSI is cycled once again, and a single picture is taken
of Callisto, viewing that portion of the satellite that perpetually points
towards Jupiter. This picture will capture the Lofn and Heimdall regions of
Callisto near the terminator, or day-night boundary, of the satellite. This
image will help to determine the relative geological ages of the regions,
as well as examine the transition between two different terrain types.

At 11:00 p.m. PDT, the suite of Fields and Particles instruments (the
Energetic Particle Detector, Magnetometer, Heavy Ion Counter, Plasma Wave,
and Plasma instruments) complete their configurations in preparation for
tomorrow's close pass by Jupiter and Io, and begin collecting and
transmitting to Earth real-time science data. This continuous real-time
data collection will span 59 hours during this sequence, concluding Tuesday
morning about 10 a.m. PDT.

-----
Note 1. Pacific Daylight Time (PDT) is 7 hours behind Greenwich Mean Time
(GMT). The time when an event occurs at the spacecraft is known as
Spacecraft Event Time (SCET). The time at which radio signals reach Earth
indicating that an event has occurred is known as Earth Received Time
(ERT). Currently, it takes Galileo's radio signals 49 minutes to travel
between the spacecraft and Earth. All times quoted above are in Earth
Received Time.

For more information on the Galileo spacecraft and its mission to Jupiter,
please visit the Galileo home page at one of the following URL's:

http://galileo.jpl.nasa.gov
http://www.jpl.nasa.gov/galileo


JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF.
http://www.jpl.nasa.gov

Enrico Piazza

ETNA VOLCANO: UPDATE FROM SPACE

Mount Etna, Europe's most active volcano, continues to spill rivers of lava
following a July 17 eruption. The recent activity of the 3,315-meter (10,876-foot) high
volcano can be seen in two images taken Sunday, July 29 by the Advanced Spaceborne
Thermal Emission and Reflection Radiometer on NASA's Terra spacecraft.

The images are available at:

http://www.jpl.nasa.gov/images/earth/volcano .

One image shows the lava advancing toward the town of Nicolosi on the Italian
island of Sicily. While the last two days have been relatively calm, a river of lava is about
4 kilometers (2.5 miles) away from the town. Thick ash clouds caused airport closures
and forced residents in the nearby city of Catania to use umbrellas while walking outside.
The other image shows a large sulfur dioxide plume coming from the summit of the
volcano.

More information on Advanced Spaceborne Thermal Emission and Reflection
Radiometer is available at:

http://asterweb.jpl.nasa.gov.

The Terra spacecraft, the flagship of a fleet of satellites dedicated to
understanding our global environment, is part of NASA's Earth Sciences Enterprise, a
long-term research program dedicated to understanding how human-induced and natural
changes affect our world. JPL is managed by the California Institute of Technology in
Pasadena.


John F. Kennedy Space Center
Kennedy Space Center, Florida 32899

KSC
Joel Wells

KSC Release No: 95-01

GENESIS NEXT PLANNED LAUNCH OPPORTUNITY AUG. 12

The launch of NASA's Genesis spacecraft aboard a Boeing Delta II
rocket was postponed again today because of unacceptable weather conditions.
Launch is now scheduled to occur at 12:08:13 p.m. EDT, Sunday, Aug.12.

Mission managers today officially reserved Aug. 12 and 13 on the
Eastern Range, and will consider any earlier opportunities that become
available. The near term Genesis launch period extends to Aug. 15. The Delta
II rocket and Genesis spacecraft remain in excellent health.

Genesis will be NASA's first sample return mission of this millennium, when
it captures a piece of the Sun and returns to Earth. It will travel to a
point where the Sun and Earth gravities are balanced, open its collector
arrays and capture elements in the solar wind. The samples will help
scientists learn about the beginnings of our solar system.


John F. Kennedy Space Center
Kennedy Space Center, Florida 32899

KSC Bruce Buckingham

KSC Release No. 94 - 01
MISSION STS-105 EVENTS, KSC NEWS CENTER OPERATING HOURS SET

News conferences, events and operating hours for KSC's News Center
have been set for the launch of the Space Shuttle Discovery on mission
STS-105, the 106th launch in the Shuttle program. The preferred time for
launch on Thursday, Aug. 9 is about 5:38 p.m. EDT at the opening of a window
that extends for about 5 minutes. The news conferences and events listed
below will be carried live on NASA Television (unless otherwise noted) and
originate from the KSC News Center.

The four-member STS-105 crew and the three-member Expedition Three
crew will arrive at KSC on Sunday, Aug. 5, at about 12:30 p.m. EDT. News
media representatives planning to cover the event must be at the KSC News
Center by 11:30 a.m. (in the event of a possible early crew arrival) to be
transported to the Shuttle Landing Facility.

On launch day, the crew will depart their KSC living quarters and be driven
to the launch pad at about 1:47 p.m. Media interested in attending this
event should be at the KSC News Center no later than 12:45 p.m.

In addition to daily 9 a.m. countdown status briefings, a prelaunch
press conference will be held two days before launch. The full briefing
schedule is listed below.

News media representatives with proper authorization may obtain
STS-105 mission credentials at the Pass and Identification Building on State
Road 3 (south of KSC) on Merritt Island during published times. Credential
and badging hours are listed below.

STS-105 BRIEFINGS & EVENTS SCHEDULE (all times are EDT)
(All briefings are held inside the KSC Press Site auditorium and will be
carried live on NASA TV unless otherwise noted)

L-4 Days - Sunday, Aug. 5
12:30 p.m. ----- STS-105 Flight Crew Arrival (Live on NASA TV)

L-3 Days - Monday, Aug. 6
9 a.m. ------ Countdown Status Briefing
* Steve Altemus, NASA Test Director
* Glenn Chin, STS-105 Mission Manager
* Ed Priselac, Shuttle Weather Officer
*
* 5 p.m. - Launch countdown begins
*
* L-2 Days - Tuesday, Aug. 7
* 9 a.m. ------ Countdown Status Briefing
* Pete Nickolenko, NASA Test Director
* Glenn Chin, STS-105 Mission Manager
* Ed Priselac, Shuttle Weather Officer
*
* 4 p.m. ----- Prelaunch News Conference
* Ron Dittemore, Shuttle Program Manager, NASA, JSC
* Bill Gerstenmaier, Deputy Manager, ISS Program, NASA, JSC
* Dave King, Director of Shuttle Processing, NASA, KSC
* John Weems, Launch Weather Officer
*
* L-1 Day - Wednesday, Aug. 8
* 9 a.m. ------ Countdown Status Briefing
* Steve Altemus, NASA Test Director
* Glenn Chin, STS-105 Mission Manager
* Ed Priselac, Shuttle Weather Officer
*
* L-0 Day - Thursday, Aug. 9
* (Tanking begins at about 8:42 a.m.)
* 12 Noon ----- NASA Television live launch programming and commentary
begins
*
* Launch Day Crew activities:
7:30 a.m. --------Wake up
* 8 a.m. -------------Breakfast
* 12 noon --------- Lunch
* *12:30 p.m. -----Crew Photo
* 1:07 p.m. --------Weather briefing
* *1:30 p.m. -------Suit-up photo
* *1:47 p.m. ------ Walkout/depart for pad
* *2:17 p.m. ------ Arrive at pad
* *3:32 p.m. ------Close hatch
* *5:38 p.m. ------ Launch of Discovery
* (* Carried live on NASA TV)
*
* 6:30 p.m. ----- Post-launch Press Conference
* Jim Halsell, Shuttle Program Launch Integration Manager, KSC
* Mike Leinbach, Shuttle Launch Director, KSC

KSC News Center office hours for STS-105
(Times may be adjusted in real time depending on mission events and
timelines.)

Sunday, Aug 5........................ 11 a.m. - 2 p.m.
Monday, Aug. 6........................ 8 a.m. - 4:30 p.m.
Tuesday, Aug. 7...................... 8 a.m. - 7 p.m.
Wednesday, Aug. 8.................. 8 a.m. - 10 p.m.
Thursday, Aug. 9 (Launch Day)... 7 a.m. - 8 p.m.
* [FOR MISSION DAY SCHEDULES SEE NOTE BELOW]
Tuesday, Aug. 21 (Landing day)... 8 a.m. -- 7 p.m.

* NOTE: The KSC News Center will support media questions for
overnight and weekend STS-105 Mission Status Briefings and the in-flight
crew news conference. Media interested in attending the briefings that occur
after normal office hours (8 a.m. - 4:30 p.m. Monday-Friday), MUST make
their intentions known to the KSC News Room at least 24 hours in advance, in
order to secure proper access to the press site. Times of these briefings
are available in the NASA TV schedule at:
http://www.spaceflight.nasa.gov/realdata/nasatv/schedule.html

Pass and Identification Hours
Sunday, Aug. 5 ----------------------------- 10 - 11:30 a.m.
Monday, Aug. 6 ----------------------------- 8 a.m. - 12 noon
Tuesday, Aug. 7 ---------------------------- 8 a.m. - 12 noon
Wednesday, Aug. 8 ----------------------- 8 a.m. -- 3:30 p.m.
Thursday, Aug. 9 (Launch day)---------- 7 a.m. -- 4:30 p.m.

News media may obtain STS-105 mission credentials at the Pass and
Identification Building at Gate 2 on State Road 3, Merritt Island, during
the above published times.

News media with annual Shuttle credentials are reminded to sign the
logbook at the query counter in the News Center.

NEWS MEDIA ARE REQUIRED TO BE UNDER PUBLIC AFFAIRS ESCORT AT ALL
TIMES WHILE AT KSC EXCEPT WHEN DRIVING TO THE NEWS CENTER OR THE COMPLEX 39
CAFETERIA.

NEWS MEDIA ARE ALLOWED AT THE PRESS SITE ONLY WHEN THE KSC NEWS
CENTER IS OPEN.

Status reports and other NASA publications are available on the
World Wide Web at:
http://www-pao.ksc.nasa.gov/kscpao/kscpao.htm .

Information about the countdown and mission can be accessed
electronically via the Internet at:
http://www.ksc.nasa.gov/shuttle/countdown/ and at
http://spaceflight.nasa.gov/

For updates on future shuttle missions, visit:
http://www-pao.ksc.nasa.gov/kscpao/schedule/schedule.htm


John F. Kennedy Space Center
Kennedy Space Center, Florida 32899

Joel Wells

KSC Release No: 96-01

LAUNCH COUNTDOWN FOR SHUTTLE MISSION STS-105 BEGINS AUGUST 6

NASA will begin the countdown for launch of Space Shuttle Discovery
on mission STS-105 Aug. 6 at 5 p.m. EDT at the T-43 hour mark. This mission
marks the 11th Shuttle flight to the International Space Station and the 5th
Shuttle mission this year. The KSC launch team will conduct the countdown
from Firing Room 3 of the Launch Control Center.

The countdown includes 29 hours and 32 minutes of built-in hold time
leading to a preferred launch time at about 5:38 p.m. on Aug. 9 with a
launch window not to exceed 5 minutes. The exact location of the orbiting
International Space Station (ISS) will be determined during the T-9 minute
built-in hold. The launch director will at that time determine the exact
time of launch.

Mission STS-105 is the 30th flight of the orbiter Discovery and the 106th
flight overall in NASA's Space Shuttle program. STS-105 is scheduled to last
about 12 days with a planned KSC landing at about 1:17 p.m. on Aug. 21.

Discovery rolled into KSC's Orbiter Processing Facility on March 21,
2001, after completing mission STS-105. The orbiter rolled out of OPF bay 2
and into the VAB on June 13. While in VAB high bay 3, Discovery was mated to
the external tank and solid rocket boosters. The entire Space Shuttle stack
was transferred to Launch Pad 39A on July 2.

On mission STS-105, the seven-member crew will berth the 4.5-ton
Leonardo Multi-Purpose Logistics Module (MPLM) to the International Space
Station. Leonardo, which will be used to carry laboratory racks filled with
equipment, experiments and supplies to and from the Station, will be
attached to the Station using the Shuttle's robot arm. The Early Ammonia
Servicer (EAS) tank, which will provide intermediate ammonia resupply to the
Station's cooling system, will be installed during two spacewalks. The
three-member Expedition Two ISS crew will return to Earth following eight
days of docked operations and will be replaced by the three-member
Expedition Three crew.

The STS-105 crew includes Commander Scott Horowitz, Pilot Rick
Sturckow, and Mission Specialists Patrick Forrester and Daniel Barry, as
well as Frank Culbertson, Vladimir Nikolaevich Dezhurov and Mikhail Tyurin,
the Expedition Three crew members.

(end of general release)

COUNTDOWN MILESTONES
*all times are Eastern
Launch-3 Days (Monday, Aug. 6)

* Prepare for the start of the STS-105 launch countdown
* Perform the call-to-stations (4:30 p.m.)
* Countdown begins at the T-43 hour mark (5 p.m.)
* Begin final vehicle and facility close-outs for launch
* Check out back-up flight systems
* Review flight software stored in mass memory units and display
systems
* Load backup flight system software into Discovery's general purpose
computers
*
* Launch-2 Days (Tuesday, Aug. 7)
*
* Remove mid-deck and flight-deck platforms (12 a.m.)
* Activate and test navigational systems (10 a.m.)
* Complete preparation to load power reactant storage and distribution
system (1 p.m.)
* Flight deck preliminary inspections complete (1 p.m.)
*
* Enter first built-in hold at T-27 hours for duration of 8 hours (9
a.m.)
*
* Clear launch pad of all non-essential personnel
* Perform test of the vehicle's pyrotechnic initiator controllers (2
p.m.)
*
* Resume countdown (5 p.m.)
*
* Begin operations to load cryogenic reactants into Discovery's fuel
cell storage tanks
* (5 p.m. - 12 a.m.)
*
* Launch-1 Day (Wednesday, Aug. 8)
*
* Enter 4-hour built-in hold at T-19 hours (1 a.m.)
*
* Demate orbiter mid-body umbilical unit (1:30 a.m.)
*
Resume countdown (5 a.m.)
*
* Final preparations of the Shuttle's three main engines for main
propellant tanking and flight (5 a.m.)
* Begin filling pad sound suppression system water tank (7:30 a.m.)
* Resume orbiter and ground support equipment close-outs
* Pad sound suppression system water tank filling complete (12:30
p.m.)
* Close out the tail service masts on the mobile launcher platform

*
Enter planned hold at T-11 hours for 12 hours, 42 minutes (1 p.m.)
*
* Begin star tracker functional checks (1:30 p.m.)
* Activate orbiter's inertial measurement units
* Activate the orbiter's communications systems
* Install film in numerous cameras on the launch pad (3:30 p.m.)
* Flight crew equipment late stow (5:30 p.m.)
* Move Rotating Service Structure (RSS) to the park position (9:30
p.m.)
* Perform ascent switch list
* Fuel cell flow-through purge complete
*
* Launch Day (Thursday, Aug. 9)
*
* Resume countdown at T-11 hours (1:42 a.m.)
*
* Activate the orbiter's fuel cells (2:52 a.m.)
* Clear the blast danger area of all non-essential personnel
* Switch Discovery's purge air to gaseous nitrogen (3:57 a.m.)
*
* Enter planned 2-hour built-in hold at the T-6 hour mark (6:42 a.m.)
*
* Launch team verifies no violations of launch commit criteria prior
to cryogenic loading of the external tank
* Clear pad of all personnel
* Chilldown of propellant transfer lines (8:12 a.m.)
* Begin loading the external tank with about 500,000 gallons of
cryogenic propellants (about 8:42 a.m.)
*
* Resume countdown (8:42 a.m.)
*
* Complete filling the external tank with its flight load of liquid
hydrogen and liquid oxygen propellants (about 11:42 a.m.)
* Final Inspection Team proceed to launch pad
*
* Enter planned 2-hour built-in hold at T-3 hours (11:42 a.m.)
*
* Perform inertial measurement unit preflight calibration
* Align Merritt Island Launch Area (MILA) tracking antennas
* Perform open loop test with Eastern Range
*
* Resume countdown at T-3 hours (1:42 p.m.)
*
* Crew departs Operations and Checkout Building for the pad (1:47
p.m.)
* Complete close-out preparations in the white room
* Check cockpit switch configurations

* Flight crew begins entry into the orbiter (about 2:17 p.m.)
* Astronauts perform air-to-ground voice checks with Launch and
Mission Control
* Close Discovery's crew hatch (about 3:32 p.m.)
* Begin Eastern Range final network open loop command checks
* Perform hatch seal and cabin leak checks
* Complete white room close-out
* Close-out crew moves to fallback area
* Primary ascent guidance data is transferred to the backup flight
system
*
* Enter planned 10-minute hold at T-20 minutes (4:22 p.m.)
*
* NASA Test Director conducts final launch team briefings
* Complete inertial measurement unit preflight alignments
*
* Resume countdown at T-20 minutes (4:32 p.m.)
*
* Transition the orbiter's onboard computers to launch configuration
* Start fuel cell thermal conditioning
* Close orbiter cabin vent valves
* Transition backup flight system to launch configuration
*
* Enter estimated 40-minute hold at T-9 minutes (4:43 p.m.)
*
* Launch Director, Mission Management Team and NASA Test Director
conduct final polls for go/no go to launch
*
* Resume countdown at T-9 minutes (about 5:23 p.m.)
*
* Start automatic ground launch sequencer (T-9:00 minutes)
* Retract orbiter crew access arm (T-7:30)
* Start mission recorders (T-6:15)
* Start Auxiliary Power Units (T-5:00)
* Arm SRB and ET range safety safe and arm devices (T-5:00)
* Start liquid oxygen drainback (T-4:55)
* Start orbiter aerosurface profile test (T-3:55)
* Start main engine gimbal profile test (T-3:30)
* Pressurize liquid oxygen tank (T-2:55)
* Begin retraction of the gaseous oxygen vent arm (T-2:55)
* Fuel cells to internal reactants (T-2:35)
* Pressurize liquid hydrogen tank (T-1:57)
* Deactivate SRB joint heaters (T-1:00)
* Orbiter transfers from ground to internal power (T-0:50 seconds)
* Ground Launch Sequencer go for auto sequence start (T-0:31 seconds)
* SRB gimbal profile (T-0:21 seconds)
* Ignition of three Space Shuttle main engines (T-6.6 seconds)
* SRB ignition and liftoff (T-0)

SUMMARY OF BUILT-IN HOLDS FOR STS-105

T-TIME LENGTH OF HOLD HOLD BEGINS HOLD ENDS
T-27 hours 8 hours 9 a.m. Tues. 5 p.m. Tues.
T-19 hours 4 hours 1 a.m. Wed. 5 a.m. Wed.
T-11 hours 12 hours, 42 minutes 1 p.m. Wed. 1:42 a.m. Thurs.

T-6 hours 2 hours 6:42 a.m. Thurs. 8:42 a.m. Thurs.
T-3 hours 2 hours 11:42 a.m. Thurs. 1:42 p.m. Thurs.
T-20 minutes 10 minutes 4:22 p.m. Thurs. 4:32 p.m. Thurs.

T-9 minutes about 40 minutes 4:43 p.m. Thurs. 5:23 p.m.
Thurs.

 

CREW FOR MISSION STS-105
Commander (CDR): Scott Horowitz
Pilot (PLT): Rick Sturckow
Mission Specialist 1: Patrick Forrester
Mission Specialist 2: Daniel Barry
Expedition Three CDR: Frank Culbertson
Expedition Three: Mikhail Tyurin
Expedition Three: Vladimir Dezhurov

SUMMARY OF STS-105 LAUNCH DAY CREW ACTIVITIES

Thursday, August 9
7:30 a.m. Crew wake up
8 a.m. Breakfast
9:30 a.m. Medical checks
12:00 p.m. Lunch
*12:30 p.m. Photo opportunity
1:07 p.m. Weather Briefing (CDR, PLT, MS2)
1:07 p.m. Don flight suits (MS1, MS3, MS4, MS5)
*1:17 p.m. Don flight suits (CDR, PLT, MS2)
*1:47 p.m. Depart for launch pad
*2:17 p.m. Arrive at white room and begin ingress
*3:32 p.m. Close crew hatch
*5:38 p.m. Launch

* Televised events (times may vary slightly)
All times Eastern


August 3, 2001


Kathleen Burton Aug. 3, 2001
NASA Ames Research Center, Moffett Field, CA

Release: 01-54AR

NASA Scientists Propose New Theory of Earth's Early Evolution

NASA scientists recently proposed a new explanation for the rise of oxygen in Earth's early atmosphere - an event that may have jumpstarted the evolution of complex life.

The idea is suggested in two research papers from NASA's Ames Research Center in the heart of California's Silicon Valley. Both papers address how the Earth got its oxygen-rich atmosphere. One uses theoretical models and the other measurements of 'microbial mats,' communities of microorganisms similar to those found on early Earth. The papers are "The Role of Microbial Mats in the Production of Reduced Gases on Early Earth," by Tori Hoehler, et al., and "Biogenic Methane, Hydrogen Escape, and the Irreversible Oxidation of Early Earth," by David Catling, et al. They were published in the July 19 issue of Nature and the Aug. 3 issue of Science, respectively.

Catling's team argues that oxygen increased in Earth's atmosphere more than 2 billion years ago because hydrogen atoms from water hitched a one-way ride into space inside methane gas produced by primitive microbes. This irreversible loss of hydrogen, they say, left behind an excess of oxygen, which gradually filled the Earth's crust and then flooded Earth's atmosphere.

"Without oxygen, the most sophisticated life on Earth would have been green microbial scum," said Catling. "Fortunately, some bacteria in the early oceans were able to separate water into hydrogen and oxygen. The hydrogen was lost to space, leaving the oxygen behind."

Before 2.4 billion to 2.2 billion years ago, the Earth's atmosphere contained almost no oxygen and could support only single-celled forms of life. The first complicated cells, like the ones that make up today's plants and animals, appear in 2.1 billion-year-old fossils just after the rise of oxygen.

Hoehler and his team measured gases released from modern microbial mats in Baja, Mexico, under conditions simulating the early atmosphere. These mats are close cousins to those that once made up much of the early Earth's biosphere. The team found that the mats released large amounts of hydrogen at night. "If the Earth's early microbial mats acted similarly to the modern ones we studied, they may have pumped a thousand times more hydrogen into the atmosphere than did volcanoes and hydrothermal vents, the other main sources," Hoehler said.

Hoehler and his co-authors suggest that some of the hydrogen might have escaped directly to space, while the remainder could have provided an important food source for other microbes - such as those that produce methane. "We found that the elevated levels of hydrogen within the mats favor the biological production and release of methane. This supports the premise of Dr. Catling's work," Hoehler said. But either way, hydrogen escaped and the Earth became more oxidized.

Questions of how and why oxygen built up in the Earth's atmosphere have been controversial for decades. Although scientists have ample evidence that oxygen first appeared in the atmosphere a little more than 2 billion years ago, why this happened has long been the subject of speculation. Fundamentally, the oxygen in the air is a byproduct of photosynthesis. In photosynthesis, plants and microbes use sunlight to steal hydrogen from water. The hydrogen is mostly used to make organic matter from carbon dioxide and the unwanted oxygen is released. But microbes that make oxygen in photosynthesis were living on Earth at least a half-billion years before oxygen first flooded the atmosphere.

For oxygen to stay in the atmosphere, the hydrogen and oxygen (or the organic matter made from the hydrogen) must be kept apart. Otherwise, they will react with each other and the oxygen will disappear. Conventional theories have focused on the burial of dead organic matter deep in the Earth, where it is 'hidden' from atmospheric oxygen. The possibility that a lot of hydrogen might escape to space was largely ignored.

According to Catling, his theory of high levels of hydrogen-containing methane gas, which acquired its hydrogen indirectly from water, also would account for why early Earth didn't freeze. "Three billion years ago, the sun was only 4/5ths as bright as it is now. The Earth should have frozen over," he said. But methane, a powerful greenhouse gas, would have kept the Earth warm.

Related information about both papers may be obtained from:
http://www.sciencemag.org and http://www.nature.com

Other authors, all of NASA Ames Research Center, include Drs. Brad Bebout and David Des Marais on the Nature paper and Drs. Kevin Zahnle and Christopher McKay on the Science paper.

NASA's Exobiology and Astrobiology Programs provided funding for both projects.

JPL Pasadena, CA

Galileo Gets One Last Frequent-Flyer Upgrade

The resilient Galileo spacecraft doesn't know when to call it quits. So, NASA has outlined the details of one last mission extension, which includes five more flybys of the Jovian moons before a final plunge into the crushing pressure of the giant planet's atmosphere.

Galileo has been orbiting Jupiter for more than five years and survived radiation exposure more than three times what it was built to withstand. Galileo's mission has previously been extended twice and during that time it has returned an enormous wealth of scientific information, including evidence of a sub-surface ocean on Jupiter's moon Europa.

"We're proud that this workhorse of a spacecraft has kept performing well enough that we can ask it to keep serving science a little longer," commented Dr. Jay Bergstralh, Acting Director of Solar System Exploration at NASA Headquarters, Washington, DC.

On May 25, Galileo should pass about 123 kilometers (76 miles) above the moon Callisto, the second largest of Jupiter's 28 known moons. The effects of Callisto's gravity will set up the space probe for a swing over both polar regions of the intensely volcanic moon Io in August and October.

Galileo will take pictures, measure magnetic forces, and study dust and smaller particles. Science goals include studying the extent of volcanism on Io, both in new and previously active sites; determining whether Io generates its own weak magnetic field; and gaining a better understanding of a doughnut-shaped ring, the Io Torus, that encircles Jupiter and contains electrically charged gases.

In 2002, having completed its imaging mission, Galileo will continue studies of Jupiter's massive magnetic field with seven instruments. In January, the orbiter will fly near the equator of Io.

In November, it will swing closer to Jupiter than ever before, dipping within about 500 kilometers (about 300 miles) of the moon Amalthea, which is less than one-tenth the size of Io and less than half as far from Jupiter. Scientists will use Galileo measurements to determine the mass and density of Amalthea. They will also study dust particles as Galileo flies through Jupiter's gossamer rings and seek new details of the magnetic forces and the densities of charged particles close to the planet.

Galileo's final orbit will take an elongated loop away from Jupiter. Then in August 2003, the spacecraft will head back for a direct impact and burn up as it plows into Jupiter's 60,000 kilometer-thick atmosphere. This final act was approved by the National Research Council of the National Academy of Sciences last December.

"Galileo has already succeeded beyond expectations, and we have the opportunity to learn still more in coming months, but it is sad to see the end of the road up ahead," said Eilene Theilig, Galileo project manager at NASA's Jet Propulsion Laboratory, Pasadena, CA. "Exposure from Jupiter's intense radiation belts has impaired some of Galileo's instruments, but it is still producing valuable scientific results."

The science program for the Galileo mission extension was recommended to NASA by a blue-ribbon panel of planetary scientists, who met last July, and will cost $9 million. "This mission extension accomplishes the highest priorities of the review panel in a cost effective way," said Paul Hertz, Galileo Program Executive at NASA Headquarters.

Galileo was launched Oct. 18, 1989, aboard NASA's Space Shuttle Atlantis. On Dec. 7, 1995, a probe released earlier from Galileo made measurements while dropping through Jupiter's upper atmosphere. Galileo's top scientific accomplishments include:

* Produced strong evidence that Europa has a melted saltwater ocean under the ice layer on its surface. The spacecraft has also found indications that Ganymede and Callisto have layers of liquid saltwater, too.
* Detailed the varied and extensive volcanic processes on Io, catching plumes erupting, fire fountains in process and lava flows expanding, among other observations.
* Delivered a probe that made the first measurements of Jupiter's atmosphere from within the atmosphere.
* Made the first close approach to an asteroid and made the first discovery of a satellite orbiting an asteroid.
* Discovered the first internal magnetic field of a moon. Ganymede's intrinsic magnetic field actually creates a "mini- magnetosphere" embedded within Jupiter's vast magnetosphere.
* Provided the only direct observation of Comet Shoemaker- Levy's impact into Jupiter.


NASA Marshall Space Flight Center
Huntsville, Ala. 35812

RELEASE: 01-261

INTERNATIONAL SPACE STATION
Expedition Two Science Operations
Status Report for the week ending Aug. 2, 2001

The Space Station crew and ground teams are preparing to conclude
one successful science expedition and begin another.

"We're coming down the home stretch for Expedition Two, with a few
activities remaining before we return the rest of the science on 7A.1
Shuttle mission," said John Uri, lead increment scientist for Expeditions
Two and Three, from NASA's Johnson Space Center in Houston. "And now we're
gearing up to begin the research on Expedition 3."

The 7A.1 Station mission, scheduled for an August 9 launch, will
carry the Expedition Three crew to the orbiting research facility and return
home with the Expedition Two crew after a five month tour of duty in space.

Three Expedition Two experiments returned home aboard Space Shuttle
Atlantis recently. Expedition Three will have 18 experiments, including 10
continuing from Expedition Two, as well as eight new experiments.

About 11 hours of crew time are allocated for remaining experiment
activities this week, not counting task list items that the crew can do as
time permits. In fact, the crew has accomplished a number of payload
activities using the task list.

"The crew has taken on the research program as their own," Uri said.
"They have been able to catch up or get ahead on work and have given up
their own time. The Expedition Two crew has set the bar very high."

On Monday, July 30, the crew completed stowing the Middeck Active
Control Experiment for return. They also received a new list of targets for
the Crew Earth Observation photography program, including a geologic fault
zone in Tanzania and the Antarctic ice sheet and icebergs near the South
Sandwich Islands. The science team confirmed that the crew was also able to
capture an image of the Mt. Etna volcano in Sicily.

They were also scheduled this week to take documentation photos of
the Protein Crystal Growth Enhanced Gaseous Nitrogen Dewar experiment, which
arrived on the recent Shuttle mission and was located in Zarya, the Russian
FGB module.

The crew this week also has continued to recharge batteries for the
Dosimetric Mapping experiment's portable radiation sensors, transfer
radiation data to a portable computer for later transmission to the ground,
and fill out their weekly questionnaire for the Interactions study dealing
with interpersonal and cultural relationships among the crew during the
Expedition.

A priority for the science team and the crew today is replacing a
possible faulty actuator on the Active Rack Isolation System, an
experimental device designed to protect delicate microgravity experiments
from vibrations caused by crew activities and powered equipment. ARIS uses
eight actuators, designed to act like powered shock absorbers to damp
vibrations before they reach experiments. Ground controllers have been
running tests of the device with seven actuators to demonstrate its fault
tolerance.

Telescience activities controlled by scientists on the ground, are
continuing with a pair of vibration measuring experiments - the Microgravity
Acceleration Measurement System and the Space Acceleration Measurement
System, as well as the Physics of Colloids in Space experiment.

Transition activities continue as the Expedition Three cadre at the
Payload Operations Center prepares to take over for Expedition Two
controllers on August 6. Controllers are continuing to update the software
on board the Station to recognize the new payloads, and control software on
the ground is undergoing similar updates.

HUBBLE PHOTOGRAPHS WARPED GALAXY AS CAMERA PASSES MILESTONE

The Hubble telescope has captured an image of an unusual edge-on
galaxy, revealing remarkable details of its warped dusty disk and
showing how colliding galaxies spawn the formation of new generations
of stars. The dust and spiral arms of normal spiral galaxies, like our
own Milky Way, appear flat when viewed edge-on. This Hubble Heritage
image of ESO 510-G13 shows a galaxy that, by contrast, has an unusual
twisted disk structure, first seen in ground-based photographs.

Image Credit: NASA and the Hubble Heritage Team (STScI/AURA)
Acknowledgment: C. Conselice (U. Wisconsin/STScI)

To see and read more, please click on:
http://heritage.stsci.edu and
http://oposite.stsci.edu/pubinfo/pr/2001/23 and links in
http://oposite.stsci.edu/pubinfo/latest.html
http://oposite.stsci.edu/pubinfo/pictures.html and
http://hubble.stsci.edu/go/news


Strange things happen to the body when humans venture into space

Strange things happen to the body when humans venture into space and the
familiar pull of gravity vanishes. Scientists say exercise is the key to
adapting to life in orbit -- and returning to Earth. This story describes
some of the reactions of the human body to weightlessness and the unusual
contraptions astronauts use to workout in space.

FULL STORY at

http://science.nasa.gov/headlines/y2001/ast02aug_1.htm?list448368


August 2, 2001

DISCOVERY SET TO LAUNCH NEXT
SPACE STATION ASSEMBLY PHASE AUG. 9

Space Shuttle Discovery will launch a new crew and a
host of supplies and scientific racks and experiments to the
International Space Station Aug. 9, beginning a new phase of
station assembly that will expand the complex as research
work grows.

Discovery's launch on the 12-day STS-105 mission has been set
for 5:38 p.m. EDT Aug. 9.

"This flight is representative of many shuttle missions to
come as station assembly and operations enter a new phase,"
Space Shuttle Program Manager Ron Dittemore said. "Although
extremely complex and challenging assembly flights will
continue, they'll be interspersed with missions dedicated to
changing station crews, experiments and supplies. Discovery
is set to launch only about two weeks after Atlantis' return
from the station, and the team has done a tremendous job."

Discovery will be commanded by astronaut Scott Horowitz
(Col., USAF). Frederick "Rick" Sturckow (Major, USMC) will be
the space shuttle's pilot. The shuttle crew also includes
Patrick Forrester (Lt. Col., USA) and Dr. Daniel Barry,
mission specialists who will perform two spacewalks during
the mission to install logistical equipment and prepare for
future station assembly.

Launching to the station aboard Discovery will be the
Expedition Three crew, led by American Commander Frank
Culbertson, and joined by Russian crewmates Vladimir
Dezhurov, mission pilot, and flight engineer Mikhail Tyurin.

The station's second resident crew, directed by Russian
Commander Yury Usachev, with American astronauts Jim Voss and
Susan Helms, will return to Earth aboard Discovery, ending
more than five months in orbit.

Discovery is expected to land about 1:17 p.m. EDT Aug. 21 at
NASA's Kennedy Space Center, FL.

Additional information about the launch of STS-105 and the
International Space Station is available on the Internet at:

http://www.shuttlepresskit.com/STS-105/index.htm

http://spaceflight.nasa.gov

http://www-pao.ksc.nasa.gov/kscpao/shuttle/countdown

Latest Scientific Advances Featured at International Tsunami Symposium

The Commerce Department's National Oceanic and Atmospheric Administration
(NOAA) will bring together the world's foremost tsunami research scientists
and mitigation engineers to discuss technical advances and progress in
tsunami science at the International Tsunami Symposium held at the
University of Washington in Seattle. Participants will discuss topics of
tsunami generation, prediction, simulation, warning, preparedness,
instrumentation and observations.

University of Washington
Kane Hall, Room 210
Seattle, Wash.

Tuesday, August 7
1996 Plan Review, 8:30 a.m. - 6 p.m.

Wednesday, August 8 - Thursday, August 9
International Symposium, 8 a.m. - 6 p.m.

Friday, August 10
Field Trip to site of the 1700 Cascadia earthquake and tsunami zone 8
a.m. - 9 p.m. (The field trip includes a canoe trip along the Copalis
River, a public forum with local officials and international tsunami
experts, and dinner on the beach.)

Joel Wells

KSC Release No: 93-01

NEXT GENESIS LAUNCH OPPORTUNITY AUG. 3

The launch of NASA's Genesis spacecraft aboard a Boeing Delta II
rocket was postponed again this morning because of unacceptable weather
conditions. Launch will now occur no earlier than 12:23:53 p.m. EDT, Friday
Aug. 3.

Workers at Launch Complex 17 tonight will prepare for fuel loading
efforts on the Delta's 1st stage, currently scheduled to begin at about 2
a.m. Friday. Mission managers will assemble for a weather update at about
5:45 a.m. Friday to determine if a launch attempt is feasible. The current
forecast indicates a 70 percent chance of weather violation at launch time
on Friday. The primary concerns are thick clouds, rain showers, and
thunderstorms.
Status reports and other NASA publications are available on the
World Wide Web at:
http://www-pao.ksc.nasa.gov/kscpao/kscpao.htm .

Information about the countdown and mission can be accessed
electronically via the Internet at:
http://www.ksc.nasa.gov/shuttle/countdown/ and at
http://www.spaceflight.nasa.gov/


SPACECRAFT TO FLY OVER SOURCE OF RECENT POLAR ERUPTION ON IO

NASA's Galileo spacecraft will buzz the north pole of Jupiter's
moon Io early next week to get unprecedented magnetic
measurements and examine the site of a dramatic recent volcanic
eruption.

The durable robot will skim about 200 kilometers (124 miles)
above Io's surface at 9:59 p.m. Aug. 5, Pacific Daylight Time
(12:59 a.m. Aug. 6, EDT). A few seconds later, Galileo will
speed over an area that was belching a giant plume of volcanic
gases seven months ago. The spacecraft will be flying at a
lower altitude than the top of the plume, creating the
possibility that Galileo will fly right through a volcanic
plume for the first time.

"Plumes in the polar regions of Io appear to be infrequent
and short-lived, so we don't know whether this one will still
be there or not," said Dr. Eilene Theilig, Galileo project manager
at NASA's Jet Propulsion Laboratory, Pasadena, Calif.

The Galileo flight team at JPL chose the polar path of
this flyby because magnetic readings above the pole might
reveal whether Io generates a surrounding magnetic field of its
own, like the magnetic field around Earth. Determining that
would add to understanding of Io's hot interior, said Dr.
Torrence Johnson, Galileo project scientist at JPL.

"All of our previous magnetic measurements at Io have been
on equatorial passes, and from those we can't tell whether the
field at Io is induced by Jupiter's strong magnetic field or
produced by Io itself," Johnson said. Polar measurements may
give enough additional information to distinguish between those
two possibilities.

As a side benefit, the path will take Galileo directly over
a dynamic volcano named Tvashtar. In November 1999, Galileo
imaged an active "curtain of fire" eruption at Tvashtar. The
volcano was hurling magma more than 1.5 kilometers (1 mile)
high. The eruption had become much less violent and had shifted
to a different part of Tvashtar by Galileo's next flyby, three
months later. Then, a tenuous gas plume from Tvashtar was
discovered from images taken by Galileo and by NASA's Cassini
spacecraft within a few days of when Cassini passed Jupiter
on its way toward Saturn on Dec. 30, 2000. The plume rose as
much as 385 kilometers (239 miles) high. Where sulfurous
material from it fell back to the surface, it created a red
ring about 1,400 kilometers (870 miles) in diameter.

If the plume is still active and the same size, Galileo will
fly through about the top quarter of it. The project's
scientists and engineers estimate that at that altitude the
plume material is very thin gas without particles large enough
to penetrate the spacecraft.

Whether the plume is active or not, Galileo will look for
changes in the Tvashtar region. "We'll be trying to figure out
just where the plume erupted from," Johnson said.

As Galileo passes Io, it will be out of communication with
Earth. NASA's Deep Space Network, which provides the
communication link for interplanetary spacecraft, has a large
antenna temporarily out of service in Spain, the only one of
the network's three sites that will have Jupiter in view above
it during the flyby. The antenna is being upgraded to help
handle an increased number of missions that will need
communications in 2003 and 2004. Confirmation of Galileo's
status during the flyby will not be received until several
hours afterwards. Images and other data from the flyby will
be returned gradually over the following two months.

Io is the innermost of Jupiter's four largest moons. Heat
from tidal flexing powered by Jupiter's gravitational pull
makes it the most volcanically active world in the solar system,
with an estimated 200 to 300 volcanoes rapidly resurfacing it.

Galileo has been orbiting Jupiter in elongated loops since 1995.
Four of its previous 31 close flybys of Jupiter's moons have
been by Io. It will swing near Io twice more after next week,
once in October and again in January, then near the small inner
moon Amalthea once before a mission-ending plunge into the
crushing pressure of Jupiter's atmosphere in 2003. Galileo's
mission was originally scheduled to end in 1997, but has been
extended three times to take advantage of the spacecraft's
durability.

The orbiter has survived more than three times the cumulative
radiation exposure it was designed to withstand. Some electronic
components have been affected by the radiation, and each loop
near Jupiter increases the odds of more serious damage from
exposure to the radiation belts around the planet, Theilig said.
Engineers have developed some new strategies for attempting to
minimize the loss of images caused by an intermittent problem
that has affected Galileo's camera since last summer.

JPL, a division of the California Institute of Technology in
Pasadena, manages Galileo for NASA's Office of Space Science,
Washington, D.C. Additional information about the mission is
available online at

http://galileo.jpl.nasa.gov


MISSION: STS-105 - 11th ISS Flight (7A.1) - Leonardo MPLM
VEHICLE: Discovery/OV-103
LOCATION: Launch Pad 39A

TARGET KSC LAUNCH DATE/TIME: Aug. 9, 2001 at 5:38 p.m. EDT
TARGET KSC LANDING DATE/TIME: Aug. 21, 2001 at about 1:17 p.m.
MISSION DURATION: 11 days, 20 hours and 25 minutes
CREW: Horowitz, Sturckow, Barry, Forrester; (ISS up) Culbertson, Dezhurov,
Tyurin; (ISS down) Usachev, Voss, Helms,
ORBITAL INSERTION ALTITUDE and INCLINATION: 122 nautical miles/51.6 degrees

Shuttle Processing Note: Following the Flight Readiness Review Wednesday,
NASA managers confirmed Aug. 9 as the official launch date for STS-105. At
Launch Pad 39A, workers have completed replacement of Discovery's master
events controller No. 2 and retests are nearing completion. Routine checks
of the spacesuits are complete also.

Orbiter aft compartment close-outs will continue into the weekend with aft
door installation scheduled for Saturday evening. Shuttle ordnance work
begins this afternoon and ordnance device installation is scheduled to occur
late tonight.

Payload Processing Note: The Integrated Vehicle Test (IVT) between the
Orbiter and the MPLM will be performed today. The payload bay doors will be
re-opened Friday evening to support Simplesat payload prelaunch operations.
The doors will be closed for flight Monday.

Upcoming Milestones
Flight crew arrival at KSC Aug. 5 (12:30 p.m.)
Launch countdown begins Aug. 6 (5 p.m.)
Begin external tank loading Aug. 9 (8:42 a.m.)

MISSION: STS-108 - 12th ISS Flight (UF1) - MPLM
VEHICLE: Endeavour/OV-105
LOCATION: Orbiter Processing Facility (OPF) bay 1
TARGET KSC LAUNCH DATE/TIME: Nov. 29, 2001 at 7:23 p.m. EST
TARGET KSC LANDING DATE/TIME: Dec. 9, 2001
MISSION DURATION: 10 days
CREW: Gorie, Kelly, Godwin, Tani; (ISS up) Onufrienko, Bursch, Walz; (ISS
down) Culbertson, Dezhurov, Tyurin
ORBITAL INSERTION ALTITUDE and INCLINATION: 122 nautical miles/51.6 degrees

Processing Note: Technicians are performing a condensate modification on
Endeavour's life support system. While the vehicle is powered down, workers
are also performing planned modifications on orbiter wiring and harnesses.
Workers will install the heads-up display No. 1 in the cockpit later this
week.

MISSION: STS-109 - HST Servicing Mission 3B
VEHICLE: Columbia/OV-102
LOCATION: OPF bay 3
TARGET KSC LAUNCH DATE/TIME: Jan. 17, 2002 at 3:52 a.m. EST
TARGET KSC LANDING DATE/TIME: Jan. 28, 2002
MISSION DURATION: TBD
CREW: Altman, Carey, Grunsfeld, Currie, Newman, Linnehan, Massimino
ORBITAL INSERTION ALTITUDE and INCLINATION: 308 nautical miles/28.5 degrees

Processing Note: Technicians are checking the orbiter's Ku-band antenna and
replacing window No. 2 today. Installation of the cross-feed line
installation for the orbiter maneuvering system and reaction control system
concludes today with flush and drain work to follow. Water spray boiler
checks begin tonight.

MISSION: STS-110 - 13th ISS Flight (8A) - ITS, SO, MT
VEHICLE: Atlantis/OV-104
LOCATION: Orbiter Processing Facility bay 2
KSC LAUNCH DATE/TIME: Feb. 28, 2002
KSC LANDING DATE/TIME: March 9, 2002
MISSION DURATION: 9 days
CREW: Bloomfield, Frick, Ross, Smith, Ochoa, Morin, Walheim
ORBITAL INSERTION ALTITUDE and INCLINATION: 122 nautical miles/51.6 degrees

Processing Note: Today, workers are removing Atlantis' three main engines
for inspection. The orbiter's forward reaction control system is undergoing
functional tests. Payload removal operations have been delayed because
weather has hindered payload canister arrival at the OPF. If weather
permits, the payload may be removed Friday.


August 1, 2001

2001 International Space Station Status Report #232001
Report # 23
Wednesday, August 1, 2001 5 p.m. CDT
Expedition Two Crew

A week and a half removed from the most recent shuttle visit to the International Space Station, the Expedition Two crew continues preparations for ending its mission aboard the complex as Discovery is readied for the STS-105 launch a week from tomorrow at 4:38 p.m. Central time to deliver supplies, logistics and the next crew to live aboard the orbiting outpost.

Almost immediately after Atlantis departed following its mission to install an addition on the home in space, station Commander Yury Usachev, and Flight Engineers Jim Voss and Susan Helms began unpacking and stowing supplies delivered by Atlantis, while at the same time beginning to prepare for the arrival of their replacement crew.

The Expedition Three crew consists of Commander Frank Culbertson, Pilot Vladimir Dezhurov and Flight Engineer Mikhail Tyurin. The three will be delivered aboard Discovery by its crew of Commander Scott Horowitz, Pilot Rick Sturckow and Mission Specialists Dan Barry and Pat Forrester.

The STS-105 and Expedition Three crews will travel to the Kennedy Space Center in Florida Sunday and the countdown begins Monday.

While Discovery,s countdown to launch to the ISS is set to begin, half a world away at the Baikonur Cosmodrome in Kazakhstan, the fifth Progress supply craft is being readied for launch Aug. 21 followed Sept. 15 by the launch of the next station component a Russian docking compartment named Pirs, the Russian word for pier.

Expedition Two Commander Yury Usachev, Voss and Helms also continue to oversee a variety of science investigations while packing for the trip home. Oversight from the ground is handled by the Payload Operations Center at NASA,s Marshall Space Flight Center in Huntsville, AL, except for the Human Research Facility, which is monitored and controlled from the Telescience Support Center (TSC) at the Johnson Space Center, Houston. For details on ISS science, visit the following website:

http://www.scipoc.msfc.nasa.gov

The International Space Station (ISS) is orbiting in excellent shape at an altitude averaging 240 miles (385 km). Sighting opportunities from the ground for many cities around the world can be viewed at:

http://spaceflight.nasa.gov/realdata/sightings/

The next ISS status report will be issued Wednesday, Aug. 8.


NASA News
National Aeronautics and
Space Administration

John F. Kennedy Space Center
Kennedy Space Center, Florida 32899

NASA Contacts:
Joel Wells, Kennedy Space Center

KSC Release No: 91-01


GENESIS LAUNCH POSTPONED AT LEAST 24 HOURS DUE TO WEATHER

The launch of NASA's Genesis spacecraft aboard a Boeing Delta II
rocket was postponed today because of thick cloud conditions in the flight
path of the launch vehicle. Launch will now occur no earlier than 12:27:09
p.m. EDT, Thursday Aug. 2.

Mission managers will assemble for a weather update at about 10 p.m.
tonight to determine the feasibility of a launch attempt tomorrow. The
current forecast indicates an 80 percent chance of weather violation
Thursday, a 60 percent chance of violation Friday and a 40 percent chance of
violation Saturday. The primary concerns are rain showers, thick clouds and
thunderstorms.

No significant technical issues were worked during the countdown and the
Delta II rocket and Genesis spacecraft remain in excellent health. The
two-minute launch window opens Friday at 12:23:53 p.m. EDT and Saturday at
12:23:40 p.m. EDT.

The thick cloud rule prohibits launch if the vehicle's flight path travels
through nontransparent clouds greater than 4,500 feet thick. Updates from
the weather reconnaissance aircraft reported clouds 8,000 feet thick in the
Delta's flight path during the final built-in hold at T-4 minutes.

JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109. TELEPHONE (818) 354-5011
http://www.jpl.nasa.gov
Enrico Piazza,




JASON 1 SATELLITE ARRIVES AT VANDENBERG AIR FORCE BASE

The Jason 1 satellite, a joint project of NASA and CNES, the French
space agency, arrived at Vandenberg Air Force Base, Calif., today to
begin final preparations for launch no earlier than Sept. 15.

Jason 1 is the follow-on to Topex/Poseidon, a U.S.-French
spacecraft that has been making precise measurements of ocean surface
topography since 1992. These data are used to map ocean currents,
improve the understanding of ocean circulation, measure global sea level
change and improve global climate forecasts.

The French-built Jason 1 spacecraft was flown from Nice, France, to
Vandenberg on an Antonov-124 cargo plane and then transported to a clean
room at Spaceport Systems International, located on the base. After
French and U.S. project members complete their final adjustments and
tests, the spacecraft will be fueled and turned over to the Boeing
Company on Aug. 22 in preparation for launch.

Jason 1 will be launched from Space Launch Complex 2 West at
Vandenberg Air Force Base atop a Delta II rocket. The rocket has a dual
payload system that allows the launch vehicle to carry two satellites at
once. Jason 1 will share part of the ride with another spacecraft called
Timed, a joint atmospheric mission of NASA and the Applied Physics
Laboratory, Laurel, Md. Jason 1 will be carried at the top of the
rocket's nose cone and will separate first.

The launch window is about 20 minutes each day. On Sept.15, the
window opens at 12:59 a.m PDT. The launch window gets earlier by about
12 minutes each day. A 10-day launch period is scheduled.

Once it reaches its final orbit, Jason 1 will assume the flight
path of Topex/Poseidon, which will move into a parallel orbit. They will
circle Earth every 112 minutes at an altitude of about 1,330 kilometers
(830 miles), measuring the surface topography of the oceans to within 4
centimeters (about 2 inches).
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News for July 2001 July News 1-10, 2001