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Friday, October 31, 2008

MRO HiRISE Images - October 29, 2008

MARS RECONNAISSANCE ORBITER HIRISE IMAGES
October 29, 2008

o Lineated Valley Fill and Lobate Debris Aprons in Deuteronilus Mensae
http://hirise.lpl.arizona.edu/PSP_009799_2205

o Wall of Crater in Capri Mensa
http://hirise.lpl.arizona.edu/PSP_009881_1670

o North Polar Layered Deposits and Dunes in Chasma Boreale
http://hirise.lpl.arizona.edu/PSP_009905_2650

o Polygon Network and Scalloped Depressions in Western Utopia Planitia
http://hirise.lpl.arizona.edu/PSP_010034_2250

All of the HiRISE images are archived here:

http://hirise.lpl.arizona.edu/

Information about the Mars Reconnaissance Orbiter is online at
http://www.nasa.gov/mro. The mission is managed by NASA's Jet Propulsion
Laboratory, a division of the California Institute of Technology, for the NASA
Science Mission Directorate, Washington, D.C. Lockheed Martin Space Systems,
of Denver, is the prime contractor and built the spacecraft. HiRISE is operated by t
he University of Arizona. Ball Aerospace and Technologies Corp., of Boulder, Colo.,
built the HiRISE instrument.

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Mars Odyssey THEMIS Images: October 27-31, 2008

MARS ODYSSEY THEMIS IMAGES
October 27-31, 2008

o Channel (Released 27 October 2008)
http://themis.asu.edu/zoom-20081027a

o Semeykin Drainage (Released 28 October 2008)
http://themis.asu.edu/zoom-20081028a

o Linear Ridges (Released 29 October 2008)
http://themis.asu.edu/zoom-20081029a

o Dust Devil Tracks (Released 30 October 2008)
http://themis.asu.edu/zoom-20081030a

o Arcuate Fractures (Released 31 October 2008)
http://themis.asu.edu/zoom-20081031a


All of the THEMIS images are archived here:

http://themis.asu.edu/latest.html

NASA's Jet Propulsion Laboratory manages the 2001 Mars Odyssey mission
for NASA's Office of Space Science, Washington, D.C. The Thermal Emission
Imaging System (THEMIS) was developed by Arizona State University,
Tempe, in co.oration with Raytheon Santa Barbara Remote Sensing.
The THEMIS investigation is led by Dr. Philip Christensen at Arizona State
University. Lockheed Martin Astronautics, Denver, is the prime contractor
for the Odyssey project, and developed and built the orbiter. Mission
operations are conducted jointly from Lockheed Martin and from JPL, a
division of the California Institute of Technology in Pasadena.

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'Ghost of Mirach' Materializes in Space Telescope Image

Feature October 31, 2008


'Ghost of Mirach' Materializes in Space Telescope Image

NASA's Galaxy Evolution Explorer has lifted the veil off a ghost known to haunt the local
universe, providing new insight into the formation and evolution of galaxies.

The eerie creature, called NGC 404, is a type of galaxy known as "lenticular." Lenticular
galaxies are disk-shaped, with little ongoing star formation and no spiral arms. NGC 404 is the
nearest example of a lenticular galaxy, and therefore of great interest. But it lies hidden in the
glare from a red giant star called Mirach. For this reason, NGC 404 became known to
astronomers as the "Ghost of Mirach."

When the Galaxy Evolution Explorer spied the galaxy in ultraviolet light, a spooky ring
materialized.

"We thought this celestial ghost was essentially dead, but we've been able to show that it has an
extended ring of new stars. The galaxy has a hybrid character in which the well-known, very old
stellar population tells only part of the story," said David Thilker of Johns Hopkins University in
Baltimore. "It's like the living dead."

Thilker and members of the Galaxy Evolution Explorer team spotted the Ghost of Mirach in
images taken during the space telescope's all-sky survey. The Galaxy Evolution Explorer is a
relatively low-cost NASA mission, launched in 2003, with an ambitious charge to survey the
entire visible sky in ultraviolet light, a job never before accomplished. Because Earth's
atmosphere absorbs ultraviolet photons -- a good thing for us living creatures who are susceptible
to the damaging light -- ultraviolet telescopes must operate from space.

The first images of the Ghost of Mirach taken by the Galaxy Evolution Explorer hinted at a
surrounding ultraviolet-bright extended structure. Subsequent, longer exposure observations
indeed show that the lenticular galaxy is surrounded by a clumpy, never-before-seen ring of
stars.

What is this mysterious ultraviolet ring doing around an otherwise nondescript lenticular galaxy?
As it turns out, previous imaging with the National Science Foundation's Very Large Array radio
telescope in New Mexico had discovered a gaseous ring of hydrogen that matches the ultraviolet
ring observed by the Galaxy Evolution Explorer. The authors of this Very Large Array study
attributed the gas ring to a violent collision between NGC 404 and a small neighboring galaxy
900 million years ago.

The ultraviolet observations demonstrate that, when the hydrogen from the collision settled into
the plane of the lenticular galaxy, stars began to form in a ghostly ring. Young, relatively hot
stars forming in stellar clusters sprinkled throughout NGC 404's ring give off the ultraviolet light
that the Galaxy Evolution Explorer was able to see.

"Before the Galaxy Evolution Explorer image, NGC 404 was thought to contain only very old
and evolved red stars distributed in a smooth elliptical shape, suggesting a galaxy well into its
old age and no longer evolving significantly," said Mark Seibert of the Observatories of the
Carnegie Institution of Washington in Pasadena, Calif. "Now we see it has come back to life, to
grow once again."

"The Ghost of Mirach has been lucky enough to get a new lease on life through the rejuvenating,
chance merger with its dwarf companion," added Thilker.

The findings indicate that the evolution of lenticular galaxies might not yet be complete. They
may, in fact, continue to form stars in a slow, piecemeal fashion as they suck the raw, gaseous
material for stars from small, neighboring galaxies. It seems the Ghost of Mirach might act more
like a vampire than a ghost.

Caltech leads the Galaxy Evolution Explorer mission and is responsible for science operations
and data analysis. NASA's Jet Propulsion Laboratory in Pasadena, Calif., manages the mission
and built the science instrument. The mission was developed under NASA's Explorers Program
managed by the Goddard Space Flight Center, Greenbelt, Md. Researchers sponsored by Yonsei
University in South Korea and the Centre National d'Etudes Spatiales (CNES) in France
collaborated on this mission.

Graphics and additional information about the Galaxy Evolution Explorer is online at
http://www.nasa.gov/galex/ and http://www.galex.caltech.edu .

Media contact: Whitney Clavin/JPL
818-354-4673

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Thursday, October 30, 2008

E-card: Happy Halloween

Cassini Scares Up a Bewitching View of Saturn

As we begin our new Equinox mission at Saturn, the Cassini-Huygens mission team sends their "best witches" for a happy, healthy and fun Halloween. We've enjoyed sharing the stunning images and exciting results of Cassini's first four years at Saturn -- and promise many more treats as we continue studying the eerie glow of Saturn's rings, the spine-tingling thunder on the planet, the hair-raising jets on Enceladus, and the murky brew on Titan.

+ Image details
http://saturn.jpl.nasa.gov/multimedia/images/image-details.cfm?imageID=3293

+ Listen to Spooky Sounds From Cassini
http://saturn.jpl.nasa.gov/news/features/feature20081028.cfm

+ Cassini home page
http://saturn.jpl.nasa.gov


+ JPL home page
http://www.jpl.nasa.gov


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NASA to Hold Small Business Symposium

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

Rhea Borja/Mark Petrovich 818-354-0850/818-393-4359
Jet Propulsion Laboratory, Pasadena, Calif.
Rhea.R.Borja@jpl.nasa.gov/Mark.Petrovich@jpl.nasa.gov

Sonja Alexander 202-358-1761
NASA Headquarters, Washington
sonja.r.alexander@nasa.gov

NEWS RELEASE: 2008-201 Oct. 30, 2008

NASA to Hold Small Business Symposium

PASADENA, Calif. -- NASA will host the inaugural Small Business Symposium and Awards
Ceremony Nov. 17-18 in Washington at the Hilton Washington, 1919 Connecticut Ave., NW.
Participation in this symposium is open to industry, academia and domestic small businesses. The
deadline to register for the symposium is Nov. 3.

The Business Opportunities Office at NASA's Jet Propulsion Laboratory in Pasadena, Calif., and
NASA's Office of Small Business Programs at NASA Headquarters in Washington are hosting the
event.

Attendees will have the opportunity to network with NASA and its prime contractors and learn how
to do business with the agency. NASA representatives will discuss plans for future Earth and space
missions as well as other agency programs, initiatives, and business opportunities. NASA will
provide information about the skills, resources and technologies needed to achieve NASA's missions,
programs and research.

Topics at this two-day event include information about NASA's Mentor-Protege Program, how
NASA's Small Business Program works, how to reach NASA's prime contractors for subcontracting
opportunities, and how small businesses can build a high-tech industrial base.

NASA's Small Business Industry and Advocate awards will be presented on the symposium's second
day. The awards recognize outstanding contributions made by NASA employees and industry
representatives to support the agency's small business program.

To register for the symposium, visit http://acquisition.jpl.nasa.gov/boo/2008sbsym/index.asp .
For more information about the NASA-JPL Small Business Symposium, contact Andrea Acosta at
andrea.e.acosta@jpl.nasa.gov or 818-354-7531.

More information about NASA's Office of Small Business Programs is at:
http://www.osbp.nasa.gov . More information about JPL's Business Opportunities Office is at:
http://acquisition.jpl.nasa.gov/boo .

JPL is managed for NASA by the California Institute of Technology in Pasadena.

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Wednesday, October 29, 2008

Phoenix Mission Status Report

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

Veronica McGregor 818-354-9452
Jet Propulsion Laboratory, Pasadena, Calif.
Veronica.mcgregor@jpl.nasa.gov

Phoenix Mission Status Report October 29, 2008

PASADENA, Calif. -- NASA'S Phoenix Mars Lander entered safe mode late yesterday in
response to a low-power fault brought on by deteriorating weather conditions. While
engineers anticipated that a fault could occur due to the diminishing power supply, the
lander also unexpectedly switched to the "B" side of its redundant electronics and shut
down one of its two batteries.

During safe mode, the lander stops non-critical activities and awaits further instructions
from the mission team. Within hours of receiving information of the safing event, mission
engineers at NASA's Jet Propulsion Laboratory, Pasadena, Calif., and at Lockheed Martin
in Denver, were able to send commands to restart battery charging. It is not likely that any
energy was lost.

Weather conditions at the landing site in the north polar region of Mars have deteriorated
in recent days, with overnight temperatures falling to --141F (-96C), and daytime
temperatures only as high as -50F (-45C), the lowest temperatures experienced so far in the
mission. A mild dust storm blowing through the area, along with water-ice clouds, further
complicated the situation by reducing the amount of sunlight reaching the lander's solar
arrays, thereby reducing the amount of power it could generate. Low temperatures caused
the lander's battery heaters to turn on Tuesday for the first time, creating another drain on
precious power supplies.

Science activities will remain on hold for the next several days to allow the spacecraft to
recharge and conserve power. Attempts to resume normal operations will not take place
before the weekend.

"This is a precarious time for Phoenix," said Phoenix Project Manager Barry Goldstein of
JPL. "We're in the bonus round of the extended mission, and we're aware that the end
could come at any time. The engineering team is doing all it can to keep the spacecraft
alive and collecting science, but at this point survivability depends on some factors out of
our control, such as the weather and temperatures on Mars."

The ability to communicate with the spacecraft has not been impacted. However, the team
decided to cancel communication sessions Wednesday morning in order to conserve
spacecraft power. The next communication pass is anticipated at 9:30 p.m. PDT
Wednesday.

Yesterday, the mission announced plans to turn off four heaters, one at a time, in an effort
to preserve power. The faults experienced late Tuesday prompted engineers to command
the lander to shut down two heaters instead of one as originally planned. One of those
heaters warmed electronics for Phoenix's robotic arm, robotic-arm camera, and thermal and
evolved-gas analyzer (TEGA), an instrument that bakes and sniffs Martian soil to assess
volatile ingredients. The second heater served the lander's pyrotechnic initiation unit,
which hasn't been used since landing. By turning off selected heaters, the mission hopes
to preserve power and prolong the use of the lander's camera and meteorological
instruments.

Originally scheduled to last 90 days, Phoenix has completed a fifth month of exploration in
the Martian arctic. As the Martian northern hemisphere shifts from summer to autumn, the
lander was expected to generate less power due to fewer hours of sunlight reaching its
solar panels. "It could be a matter of days, or weeks, before the daily power generated by
Phoenix is less than needed to operate the spacecraft," said JPL mission manager Chris
Lewicki. "We have only a few options left to reduce the energy usage."

The Phoenix mission is led by Peter Smith of the University of Arizona, Tucson, with
project management at the Jet Propulsion Laboratory and development partnership at
Lockheed Martin, Denver. International contributions come from the Canadian Space
Agency; the University of Neuchatel, Switzerland; the universities of Copenhagen and
Aarhus in Denmark; the Max Planck Institute in Germany; and the Finnish Meteorological
Institute. The California Institute of Technology in Pasadena manages JPL for NASA.

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Tuesday, October 28, 2008

NASA's Phoenix Mission Faces Survival Challenges

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

Rhea Borja/Veronica McGregor 818-354-0850/354-9452
Jet Propulsion Laboratory, Pasadena, Calif.
Rhea.R.Borja@jpl.nasa.gov
Veronica.mcgregor@jpl.nasa.gov

NEWS RELEASE: 2008-199 October 28, 2008

NASA's Phoenix Mission Faces Survival Challenges

PASADENA, Calif. -- In a race against time and the elements, engineers with NASA's
Phoenix Mars Lander mission hope to extend the lander's survival by gradually shutting
down some of its instruments and heaters, starting today.

Originally scheduled to last 90 days, Phoenix has completed a fifth month of exploration in
the Martian arctic. As expected, with the Martian northern hemisphere shifting from
summer to fall, the lander is generating less power due to shorter days and fewer hours of
sunlight reaching its solar panels. At the same time, the spacecraft requires more power to
run several survival heaters that allow it to operate even as temperatures decline.

"If we did nothing, it wouldn't be long before the power needed to operate the spacecraft
would exceed the amount of power it generates on a daily basis," said Phoenix Project
Manager Barry Goldstein of NASA's Jet Propulsion Laboratory, Pasadena, Calif. "By
turning off some heaters and instruments, we can extend the life of the lander by several
weeks and still conduct some science."

Over the next several weeks, four survival heaters will be shut down, one at a time, in an
effort to conserve power. The heaters serve the purpose of keeping the electronics within
tested survivable limits. As each heater is disabled, some of the instruments are also
expected to cease operations. The energy saved is intended to power the lander's main
camera and meteorological instruments until the very end of the mission.

Later today, engineers will send commands to disable the first heater. That heater warms
Phoenix's robotic arm, robotic-arm camera, and thermal and evolved-gas analyzer (TEGA),
an instrument that bakes and sniffs Martian soil to assess volatile ingredients. Shutting
down this heater is expected to save 250 watt-hours of power per Martian day.

The Phoenix team has parked the robotic arm on a representative patch of Martian soil. No
additional soil samples will be gathered. The thermal and electrical-conductivity probe
(TECP), located on the wrist of the arm, has been inserted into the soil and will continue to
measure soil temperature and conductivity, along with atmospheric humidity near the
surface. The probe does not need a heater to operate and should continue to send back data
for weeks.

Throughout the mission, the lander's robotic arm successfully dug and scraped Martian soil
and delivered it to the onboard laboratories. "We turn off this workhorse with the
knowledge that it has far exceeded expectations and conducted every operation asked of
it," said Ray Arvidson, the robotic arm's co-investigator, and a professor at Washington
University, St. Louis.

When power levels necessitate further action, Phoenix engineers will disable a second
heater, which serves the lander's pyrotechnic initiation unit. The unit hasn't been used since
landing, and disabling its heater is expected to add four to five days to the mission's
lifetime. Following that step, engineers would disable a third heater, which warms
Phoenix's main camera -- the Surface Stereo Imager --and the meteorological suite of
instruments. Electronics that operate the meteorological instruments should generate
enough heat on their own to keep most of those instruments and the camera functioning.

In the final step, Phoenix engineers may turn off a fourth heater -- one of two survival
heaters that warm the spacecraft and its batteries. This would leave one remaining survival
heater to run out on its own.

"At that point, Phoenix will be at the mercy of Mars," said Chris Lewicki of JPL, lead
mission manger.

Engineers are also preparing for solar conjunction, when the sun is directly between Earth
and Mars. Between Nov. 28 and Dec. 13, Mars and the sun will be within two degrees of
each other as seen from Earth, blocking radio transmission between the spacecraft and
Earth. During that time, no commands will be sent to Phoenix, but daily downlinks from
Phoenix will continue through NASA's Odyssey and Mars Reconnaissance orbiters. At
this time, controllers can't predict whether the fourth heater would be disabled before or
after conjunction.

The Phoenix mission is led by Peter Smith of the University of Arizona, Tucson, with
project management at the Jet Propulsion Laboratory and development partnership at
Lockheed Martin, Denver. International contributions come from the Canadian Space
Agency; the University of Neuchatel, Switzerland; the universities of Copenhagen and
Aarhus in Denmark; the Max Planck Institute in Germany; and the Finnish Meteorological
Institute. The California Institute of Technology in Pasadena manages JPL for NASA.

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NASA Orbiter Reveals Details of a Wetter Mars

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

Guy Webster 818-354-6278
Jet Propulsion Laboratory, Pasadena, Calif.
guy.webster@jpl.nasa.gov

Dwayne Brown 202-358-1726
NASA Headquarters, Washington
dwayne.c.brown@nasa.gov

Jennifer Huergo 240-228-5618
Johns Hopkins University Applied Physics Laboratory, Laurel, Md.
jennifer.huergo@jhuapl.edu

NEWS RELEASE: 2008-198 Oct. 28, 2008

NASA Orbiter Reveals Details of a Wetter Mars

PASADENA, Calif. -- NASA's Mars Reconnaissance Orbiter has observed a new category of
minerals spread across large regions of Mars. This discovery suggests that liquid water remained on
the planet's surface a billion years later than scientists believed, and it played an important role in
shaping the planet's surface and possibly hosting life.

Researchers examining data from the orbiter's Compact Reconnaissance Imaging Spectrometer for
Mars have found evidence of hydrated silica, commonly known as opal. The hydrated, or water-
containing, mineral deposits are telltale signs of where and when water was present on ancient Mars.

"This is an exciting discovery because it extends the time range for liquid water on Mars, and the
places where it might have supported life," said Scott Murchie, the spectrometer's principal
investigator at the Johns Hopkins University Applied Physics Laboratory in Laurel, Md. "The
identification of opaline silica tells us that water may have existed as recently as 2 billion years ago."

Until now, only two major groups of hydrated minerals, phyllosilicates and hydrated sulfates, had
been observed by spacecraft orbiting Mars. Clay-like phyllosilicates formed more than 3.5 billion
years ago where igneous rock came into long-term contact with water. During the next several
hundred million years, until approximately 3 billion years ago, hydrated sulfates formed from the
evaporation of salty and sometimes acidic water.

The newly discovered opaline silicates are the youngest of the three types of hydrated minerals.
They formed where liquid water altered materials created by volcanic activity or meteorite impact on
the Martian surface. One such location noted by scientists is the large Martian canyon system called
Valles Marineris.

"We see numerous outcrops of opal-like minerals, commonly in thin layers extending for very long
distances around the rim of Valles Marineris and sometimes within the canyon system itself," said
Ralph Milliken of NASA's Jet Propulsion Laboratory in Pasadena, Calif.

Milliken is lead author of an article in the November issue of "Geology" that describes the
identification of opaline silica. The study reveals that the minerals, which also were recently found
in Gusev Crater by NASA's Mars rover Spirit, are widespread and occur in relatively young terrains.

In some locations, the orbiter's spectrometer observed opaline silica with iron sulfate minerals, either
in or around dry river channels. This indicates the acidic water remained on the Martian surface for
an extended period of time. Milliken and his colleagues believe that in these areas, low-temperature
acidic water was involved in forming the opal. In areas where there is no clear evidence that the
water was acidic, deposits may have formed under a wide range of conditions.

"What's important is that the longer liquid water existed on Mars, the longer the window during
which Mars may have supported life," says Milliken. "The opaline silica deposits would be good
places to explore to assess the potential for habitability on Mars, especially in these younger
terrains."

The spectrometer collects 544 colors, or wavelengths, of reflected sunlight to detect minerals on the
surface of Mars. Its highest resolution is about 20 times sharper than any previous look at the planet
in near-infrared wavelengths.

NASA's Jet Propulsion Laboratory manages the Mars Reconnaissance Orbiter mission for NASA's
Science Mission Directorate in Washington. Lockheed Martin Space Systems, Denver, is the prime
contractor for the project and built the spacecraft. The Applied Physics Laboratory led the effort to
build the spectrometer and operates the instrument in coordination with an international team of
researchers from universities, government and the private sector.

More information about the Mars Reconnaissance Orbiter is at http://www.nasa.gov/mro .

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Monday, October 27, 2008

Closest Planetary System Hosts Two Asteroid Belts

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

Whitney Clavin 818-354-4673
Jet Propulsion Laboratory
whitney.clavin@jpl.nasa.gov

NEWS RELEASE: 2008-197 Oct. 27, 2008

Closest Planetary System Hosts Two Asteroid Belts

New observations from NASA's Spitzer Space Telescope indicate that the nearest planetary system to
our own has two asteroid belts. Our own solar system has just one.

The star at the center of the nearby system, called Epsilon Eridani, is a younger, slightly cooler and
fainter version of the sun. Previously, astronomers had uncovered evidence for two possible planets
in the system, and for a broad, outer ring of icy comets similar to our own Kuiper Belt.

Now, Spitzer has discovered that the system also has dual asteroid belts. One sits at approximately
the same position as the one in our solar system. The second, denser belt, most likely also populated
by asteroids, lies between the first belt and the comet ring. The presence of the asteroid belts implies
additional planets in the Epsilon Eridani system.

"This system probably looks a lot like ours did when life first took root on Earth," said Dana
Backman, an astronomer at the SETI Institute, in Mountain View, Calif., and outreach director for
NASA's Sofia mission. "The main difference we know of so far is that it has an additional ring of
leftover planet construction material." Backman is lead author of a paper about the findings to appear
Jan. 10 in the Astrophysical Journal.

Asteroid belts are rocky and metallic debris left over from the early stages of planet formation. Their
presence around other stars signals that rocky planets like Earth could be orbiting in the system's
inner regions, with massive gas planets circling near the belts' rims. In our own solar system, for
example, there is evidence that Jupiter, which lies just beyond our asteroid belt, caused the asteroid
belt to form long ago by stirring up material that would have otherwise coalesced into a planet.
Nowadays, Jupiter helps keep our asteroid belt confined to a ring.

Astronomers have detected stars with signs of multiple belts of material before, but Epsilon Eridani is
closer to Earth and more like our sun overall. It is 10 light-years away, slightly less massive than the
sun, and roughly 800 million years old, or one-fifth the age of the sun.

Because the star is so close and similar to the sun, it is a popular locale in science fiction. The
television series Star Trek and Babylon 5 referenced Epsilon Eridani, and it has been featured in
novels by Issac Asimov and Frank Herbert, among others.

The popular star was also one of the first to be searched for signs of advanced alien civilizations
using radio telescopes in 1960. At that time, astronomers did not know of the star's young age.

Spitzer observed Epsilon Eridani with both of its infrared cameras and its infrared spectrometer.
When asteroid and comets collide or evaporate, they release tiny particles of dust that give off heat,
which Spitzer can see. "Because the system is so close to us, Spitzer can really pick out details in the
dust, giving us a good look at the system's architecture," said co-author Karl Stapelfeldt of NASA's
Jet Propulsion Laboratory, Pasadena, Calif.

The asteroid belts detected by Spitzer orbit at distances of approximately 3 and 20 astronomical units
from the star (an astronomical unit is the average distance between Earth and the sun). For reference,
our own asteroid belt lies at about 3 astronomical units from the sun, and Uranus is roughly 19
astronomical units away.

One of the two possible planets previously identified around Epsilon Eridani, called Epsilon Eridani,
was discovered in 2000. The planet is thought to orbit at an average distance of 3.4 astronomical units
from the star -- just outside the innermost asteroid belt identified by Spitzer. This is the first time that
an asteroid belt and a planet beyond our solar system have been found in a similar arrangement as our
asteroid belt and Jupiter.

Some researchers had reported that Epsilon Eridani b orbits in an exaggerated ellipse ranging
between 1 and 5 astronomical units, but this means the planet would cross, and quickly disrupt, the
newfound asteroid belt. Instead, Backman and colleagues argue that this planet must have a more
circular orbit that keeps it just outside the belt.

The other candidate planet was first proposed in 1998 to explain lumpiness observed in the star's
outer comet ring. It is thought to lie near the inner edge of the ring, which orbits between 35 and 90
astronomical units from Epsilon Eridani.

The intermediate belt detected by Spitzer suggests that a third planet could be responsible for creating
and shepherding its material. This planet would orbit at approximately 20 astronomical units and lie
between the other two planets. "Detailed studies of the dust belts in other planetary systems are
telling us a great deal about their complex structure," said Michael Werner, co-author of the study
and project scientist for Spitzer at JPL. "It seems that no two planetary systems are alike."

JPL manages the Spitzer mission for NASA's Science Mission Directorate, Washington. Science
operations are conducted at the Spitzer Science Center at the California Institute of Technology in
Pasadena. Caltech manages JPL for NASA. More information about Spitzer is at
http://www.spitzer.caltech.edu/spitzer and http://www.nasa.gov/spitzer . More information about
extrasolar planets and NASA's planet-finding program is at http://planetquest.jpl.nasa.gov .

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Friday, October 24, 2008

Mars Odyssey THEMIS Images: October 20-24, 2008

MARS ODYSSEY THEMIS IMAGES
October 20-24, 2008

o Polar Dunes (Released 20 October 2008)
http://themis.asu.edu/zoom-20081020a

o Polar Dunes (Released 21 October 2008)
http://themis.asu.edu/zoom-20081021a

o Cerulli Channels (Released 22 October 2008)
http://themis.asu.edu/zoom-20081022a

o Polar Dunes (Released 23 October 2008)
http://themis.asu.edu/zoom-20081023a

o Dark Slope Streaks (Released 24 October 2008)
http://themis.asu.edu/zoom-20081024a


All of the THEMIS images are archived here:

http://themis.asu.edu/latest.html

NASA's Jet Propulsion Laboratory manages the 2001 Mars Odyssey mission
for NASA's Office of Space Science, Washington, D.C. The Thermal Emission
Imaging System (THEMIS) was developed by Arizona State University,
Tempe, in co.oration with Raytheon Santa Barbara Remote Sensing.
The THEMIS investigation is led by Dr. Philip Christensen at Arizona State
University. Lockheed Martin Astronautics, Denver, is the prime contractor
for the Odyssey project, and developed and built the orbiter. Mission
operations are conducted jointly from Lockheed Martin and from JPL, a
division of the California Institute of Technology in Pasadena.

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MRO HiRISE Images - October 22, 2008

MARS RECONNAISSANCE ORBITER HIRISE IMAGES
October 22, 2008

o Layers in Crater Wall
http://hirise.lpl.arizona.edu/PSP_009694_1545

o Linear Dunes in the North Polar Region
http://hirise.lpl.arizona.edu/PSP_009739_2580

o Fan in Holden Crater
http://hirise.lpl.arizona.edu/PSP_009841_1530

o Light-toned Layers West of Juventae Chasma
http://hirise.lpl.arizona.edu/PSP_009842_1755


All of the HiRISE images are archived here:

http://hirise.lpl.arizona.edu/

Information about the Mars Reconnaissance Orbiter is online at
http://www.nasa.gov/mro. The mission is managed by NASA's Jet Propulsion
Laboratory, a division of the California Institute of Technology, for the NASA
Science Mission Directorate, Washington, D.C. Lockheed Martin Space Systems,
of Denver, is the prime contractor and built the spacecraft. HiRISE is operated by t
he University of Arizona. Ball Aerospace and Technologies Corp., of Boulder, Colo.,
built the HiRISE instrument.

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Friday, October 17, 2008

Mars Odyssey THEMIS Images: October 13-27, 2008

MARS ODYSSEY THEMIS IMAGES
October 13-17, 2008

o Dark Slope Streaks (Released 13 October 2008)
http://themis.asu.edu/zoom-20081013a

o Gullies (Released 14 October 2008)
http://themis.asu.edu/zoom-20081014a

o Dunes (Released 15 October 2008)
http://themis.asu.edu/zoom-20081015a

o Fractures and Collapse (Released 16 October 2008)
http://themis.asu.edu/zoom-20081016a

o Lava Channel (Released 17 October 2008)
http://themis.asu.edu/zoom-20081017a


All of the THEMIS images are archived here:

http://themis.asu.edu/latest.html

NASA's Jet Propulsion Laboratory manages the 2001 Mars Odyssey mission
for NASA's Office of Space Science, Washington, D.C. The Thermal Emission
Imaging System (THEMIS) was developed by Arizona State University,
Tempe, in co.oration with Raytheon Santa Barbara Remote Sensing.
The THEMIS investigation is led by Dr. Philip Christensen at Arizona State
University. Lockheed Martin Astronautics, Denver, is the prime contractor
for the Odyssey project, and developed and built the orbiter. Mission
operations are conducted jointly from Lockheed Martin and from JPL, a
division of the California Institute of Technology in Pasadena.

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MRO HiRISE Images - October 15, 2008

MARS RECONNAISSANCE ORBITER HIRISE IMAGES
October 15, 2008

o Fan in Aeolis Region
http://hirise.lpl.arizona.edu/PSP_009623_1755

o Crater on North Polar Layered Deposits
http://hirise.lpl.arizona.edu/PSP_009663_2635

o Bacolor Crater Interior and Central Peak
http://hirise.lpl.arizona.edu/PSP_009677_2135

o Tell-Tale Rocks at Southern Acidalia Planitia
http://hirise.lpl.arizona.edu/PSP_009708_2205


All of the HiRISE images are archived here:

http://hirise.lpl.arizona.edu/

Information about the Mars Reconnaissance Orbiter is online at
http://www.nasa.gov/mro. The mission is managed by NASA's Jet Propulsion
Laboratory, a division of the California Institute of Technology, for the NASA
Science Mission Directorate, Washington, D.C. Lockheed Martin Space Systems,
of Denver, is the prime contractor and built the spacecraft. HiRISE is operated by t
he University of Arizona. Ball Aerospace and Technologies Corp., of Boulder, Colo.,
built the HiRISE instrument.

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Monday, October 13, 2008

JPL's Jon Giorgini Honored With Masursky Award

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

DC Agle 818-393-9011
Jet Propulsion Laboratory, Pasadena, Calif.
agle@jpl.nasa.gov

NEWS RELEASE: 2008-193 Oct. 13, 2008

JPL's Jon Giorgini Honored With Masursky Award

PASADENA, Calif. -- Jon Giorgini, an engineer at NASA's Jet Propulsion Laboratory,
Pasadena, Calif., has received the prestigious Harold Masursky Award, presented by the
American Astronomical Society's Division for Planetary Sciences.

The Masursky Award recognizes individuals for outstanding service to planetary science
and exploration through engineering, managerial, programmatic or public service
activities. Giorgini runs JPL's Horizons system, an online database that can generate
locations and orbits for the almost half-million known celestial bodies in our solar
system.

The award citation states in part: A specialist at the NASA Jet Propulsion Laboratory, Jon
developed and implemented the on-line Horizons system that is used by the international
scientific community to generate accurate ephemeris information for the 450,000
currently known objects in the solar system. This includes the sun, planets, their moons,
asteroids, comets, and many spacecraft… This system is used by observers, researchers,
and mission planners to plan observations and track the targets of space and ground-
based telescopes, as well as spacecraft. Since its inception in October 1996, the Horizons
system has responded to more than ten million requests (on average, more than 2200 per
day) received from 300,000 unique locations.

Giorgini, a senior engineer in JPL's Solar System Dynamics Group, was a navigator for
the Magellan spacecraft during its mapping of Venus (1991-1993), developing and
implementing the new navigation methodology for the first interplanetary aerobrake. He
created JPL's "On-Site Orbit Determination" system -- software used at the Goldstone
and Arecibo planetary radar sites to track and update the orbits of radar targets. He then
returned to navigation for the Mars Global Surveyor aerobrake planning and
interplanetary phases (1995-1997), followed by the Near-Earth Asteroid Rendezvous
mission navigation and radio science teams (1997-2001). As a member of the asteroid
radar observing team (1994-present), he is responsible for orbit analysis and predictions
used to operate radar tracking systems at Goldstone and Arecibo. He has worked on more
than 290 asteroid radar targets since 1994 and is co-discoverer of 27 asteroid satellites.
He discovered the potential Earth impact hazard posed by the asteroid 1950 DA, and
developed methods to assess dynamics and impact potential over centuries. Giorgini is
author or co-author of 99 research papers and four book chapters.

Giorgini's outside activities have included climbs of Mount Kilimanjaro and Vinson
Massif, the highest mountains in Africa and Antarctica. He has practiced martial arts and
kickboxing for the last 22 years.

Giorgini's previous awards include the JPL 2007 Ed Stone Outstanding Research Paper
Award, a NASA Space Act Award and a NASA Exceptional Service Medal. The
International Astronomical Union named asteroid "6775 Giorgini" in his honor in 1996.

Giorgini has a Bachelor of Science degree in aerospace engineering from Iowa State
University, Ames; and a Master of Science degree in aerospace engineering, specializing
in celestial mechanics, from the University of Texas, Austin. He has worked at JPL for 17
years.

For more information on JPL, visit: http://www.jpl.nasa.gov .

-end-

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NASA's Spitzer Gets Sneak Peak Inside Comet Holmes

Feature October 13, 2008



NASA's Spitzer Gets Sneak Peak Inside Comet Holmes

When comet Holmes unexpectedly erupted in 2007, professional and amateur astronomers
around the world turned their telescopes toward the spectacular event. Their quest was to find out
why the comet had suddenly exploded.

Observations taken of the comet after the explosion by NASA's Spitzer Space Telescope deepen
the mystery, showing oddly behaving streamers in the shell of dust surrounding the nucleus of
the comet. The data also offer a rare look at the material liberated from within the nucleus, and
confirm previous findings from NASA's Stardust and Deep Impact missions.

"The data we got from Spitzer do not look like anything we typically see when looking at
comets," said Bill Reach of NASA's Spitzer Science Center at the California Institute of
Technology, Pasadena, Calif. Reach is lead investigator of the Spitzer observations. "The comet
Holmes explosion gave us a rare glimpse at the inside of a comet nucleus." The findings were
presented at the 40th meeting of the Division of Planetary Sciences in Ithaca, N.Y.

Every six years, comet 17P/Holmes speeds away from Jupiter and heads inward toward the sun,
traveling the same route typically without incident. However, twice in the last 116 years, in
November 1892 and October 2007, comet Holmes exploded as it approached the asteroid belt,
and brightened a millionfold overnight.

In an attempt to understand these odd occurrences, astronomers pointed NASA's Spitzer Space
Telescope at the comet in November 2007 and March 2008. By using Spitzer's infrared
spectrograph instrument, Reach was able to gain valuable insights into the composition of
Holmes' solid interior. Like a prism spreading visible-light into a rainbow, the spectrograph
breaks up infrared light from the comet into its component parts, revealing the fingerprints of
various chemicals.

In November of 2007, Reach noticed a lot of fine silicate dust, or crystallized grains smaller than
sand, like crushed gems. He noted that this particular observation revealed materials similar to
those seen around other comets where grains have been treated violently, including NASA's
Deep Impact mission, which smashed a projectile into comet Tempel 1; NASA's Stardust
mission, which swept particles from comet Wild 2 into a collector at 13,000 miles per hour
(21,000 kilometers per hour), and the outburst of comet Hale-Bopp in 1995.

"Comet dust is very sensitive, meaning that the grains are very easily destroyed, said Reach. "We
think the fine silicates are produced in these violent events by the destruction of larger particles
originating inside the comet nucleus."

When Spitzer observed the same portion of the comet again in March 2008, the fine-grained
silicate dust was gone and only larger particles were present. "The March observation tells us
that there is a very small window for studying composition of comet dust after a violent event
like comet Holmes' outburst," said Reach.

Comet Holmes not only has unusual dusty components, it also does not look like a typical comet.
According to Jeremie Vaubaillon, a colleague of Reach's at Caltech, pictures snapped from the
ground shortly after the outburst revealed streamers in the shell of dust surrounding the comet.
Scientists suspect they were produced after the explosion by fragments escaping the comet's
nucleus.

In November 2007, the streamers pointed away from the sun, which seemed natural because
scientists believed that radiation from the sun was pushing these fragments straight back.
However, when Spitzer imaged the same streamers in March 2008, they were surprised to find
them still pointing in the same direction as five months before, even though the comet had
moved and sunlight was arriving from a different location. "We have never seen anything like
this in a comet before. The extended shape still needs to be fully understood," said Vaubaillon.

He notes that the shell surrounding the comet also acts peculiarly. The shape of the shell did not
change as expected from November 2007 to March 2008. Vaubaillon said this is because the dust
grains seen in March 2008 are relatively large, approximately one millimeter in size, and thus
harder to move.

"If the shell was comprised of smaller dust grains, it would have changed as the orientation of
the sun changes with time," said Vaubaillon. "This Spitzer image is very unique. No other
telescope has seen comet Holmes in this much detail, five months after the explosion."

"Like people, all comets are a little different. We've been studying comets for hundreds of years -
- 116 years in the case of comet Holmes -- but still do not really understand them," said Reach.
"However, with the Spitzer observations and data from other telescopes, we are getting closer."

NASA's Jet Propulsion Laboratory, Pasadena, Calif., manages the Spitzer Space Telescope
mission for NASA's Science Mission Directorate, Washington. Science operations are conducted
at the Spitzer Science Center at the California Institute of Technology, also in Pasadena. Caltech
manages JPL for NASA. For more information about Spitzer, visit
http://www.spitzer.caltech.edu/spitzer and http://www.nasa.gov/spitzer .

-end-

Media Contact: Whitney Clavin/ Jet Propulsion Laboratory
818-354-4673 whitney.clavin@jpl.nasa.gov

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Giant Cyclones at Saturn's Poles Create a Swirl of Mystery

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

Carolina Martinez 818-354-9382
Jet Propulsion Laboratory, Pasadena, Calif.
Carolina.Martinez@jpl.nasa.gov

IMAGE ADVISORY: 2008-192 Oct. 13, 2008

Giant Cyclones at Saturn's Poles Create a Swirl of Mystery

New images from NASA's Cassini spacecraft reveal a giant cyclone at Saturn's north pole, and
show that a similarly monstrous cyclone churning at Saturn's south pole is powered by Earth-like
storm patterns.

The new-found cyclone at Saturn's north pole is only visible in the near-infrared wavelengths
because the north pole is in winter, thus in darkness to visible-light cameras. At these
wavelengths, about seven times greater than light seen by the human eye, the clouds deep inside
Saturn's atmosphere are seen in silhouette against the background glow of Saturn's internal heat.

The entire north pole of Saturn is now mapped in detail in infrared, with features as small as 120
kilometers (75 miles) visible in the images. Time-lapse movies of the clouds circling the north
pole show the whirlpool-like cyclone there is rotating at 530 kilometers per hour (325 miles per
hour), more than twice as fast as the highest winds measured in cyclonic features on Earth. This
cyclone is surrounded by an odd, honeycombed-shaped hexagon, which itself does not seem to
move while the clouds within it whip around at high speeds, also greater than 500 kilometers per
hour (300 miles per hour). Oddly, neither the fast-moving clouds inside the hexagon nor this
new cyclone seem to disrupt the six-sided hexagon.

New Cassini imagery of Saturn's south pole shows complementary aspects of the region through
the eyes of two different instruments. Near-infrared images from the visual and infrared
mapping spectrometer instrument show the whole region is pockmarked with storms, while the
imaging cameras show close-up details.

The new views are available online at: http://www.nasa.gov/cassini and
http://saturn.jpl.nasa.gov.

Unlike Earth-bound hurricanes, powered by the ocean's heat and water, Saturn's cyclones have
no body of water at their bases, yet the eye-walls of Saturn's and Earth's storms look strikingly
similar. Saturn's hurricanes are locked to the planet's poles, whereas terrestrial hurricanes drift
across the ocean.


"These are truly massive cyclones, hundreds of times stronger than the most giant hurricanes on
Earth," said Kevin Baines, Cassini scientist on the visual and infrared mapping spectrometer at
NASA's Jet Propulsion Laboratory, Pasadena, Calif. "Dozens of puffy, convectively formed
cumulus clouds swirl around both poles, betraying the presence of giant thunderstorms lurking
beneath. Thunderstorms are the likely engine for these giant weather systems," said Baines.

Just as condensing water in clouds on Earth powers hurricane vortices, the heat released from the
condensing water in Saturnian thunderstorms deep down in the atmosphere may be the primary
power source energizing the vortex.

In the south, the new infrared images of the pole, under the daylight conditions of southern
summer, show the entire region is marked by hundreds of dark cloud spots. The clouds, like
those at the north pole, are likely a manifestation of convective, thunderstorm-like processes
extending some 100 kilometers (62 miles) below the clouds. They are likely composed of
ammonium hydrosulfide with possibly a mixture of materials dredged up from the depths. By
contrast, most of the hazes and clouds seen on Saturn are thought to be composed of ammonia,
which condenses at high, visible altitudes.

Complementary images of the south pole from Cassini's imaging cameras, obtained in mid-July,
are 10 times more detailed than any seen before. "What looked like puffy clouds in lower
resolution images are turning out to be deep convective structures seen through the atmospheric
haze," said Cassini imaging team member Tony DelGenio of NASA's Goddard Institute for
Space Studies in New York. "One of them has punched through to a higher altitude and created
its own little vortex."

The "eye" of the vortex is surrounded by an outer ring of high clouds. The new images also hint
at an inner ring of clouds about half the diameter of the main ring, and so the actual clear "eye"
region is smaller than it appears in earlier low-resolution images.

"It's like seeing into the eye of a hurricane," said Andrew Ingersoll, a member of Cassini's
imaging team at the California Institute of Technology, Pasadena. "It's surprising. Convection is
an important part of the planet's energy budget because the warm upwelling air carries heat from
the interior. In a terrestrial hurricane, the convection occurs in the eyewall; the eye is a region of
downwelling. Here convection seems to occur in the eye as well."

Further observations are planned to see how the features at both poles evolve as the seasons
change from southern summer to fall in August 2009.

The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency
and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California
Institute of Technology in Pasadena, manages the mission for NASA's Science Mission
Directorate, Washington, D.C. The Cassini orbiter was designed, developed and assembled at
JPL. The visual and infrared mapping spectrometer team is based at the University of Arizona.
The imaging team is based at the Space Science Institute, Boulder, Colo.

-end-


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Sunday, October 12, 2008

Mars Odyssey THEMIS Images: October 6-10, 2008

MARS ODYSSEY THEMIS IMAGES
October 6-10, 2008

o Yardangs (Released 06 October 2008)
http://themis.asu.edu/zoom-20081006a

o Polar Dunes (Released 07 October 2008)
http://themis.asu.edu/zoom-20081007a

o Collapse Features (Released 08 October 2008)
http://themis.asu.edu/zoom-20081008a

o Surface Texture (Released 09 October 2008)
http://themis.asu.edu/zoom-20081009a

o Dunes (Released 10 October 2008)
http://themis.asu.edu/zoom-20081010a


All of the THEMIS images are archived here:

http://themis.asu.edu/latest.html

NASA's Jet Propulsion Laboratory manages the 2001 Mars Odyssey mission
for NASA's Office of Space Science, Washington, D.C. The Thermal Emission
Imaging System (THEMIS) was developed by Arizona State University,
Tempe, in co.oration with Raytheon Santa Barbara Remote Sensing.
The THEMIS investigation is led by Dr. Philip Christensen at Arizona State
University. Lockheed Martin Astronautics, Denver, is the prime contractor
for the Odyssey project, and developed and built the orbiter. Mission
operations are conducted jointly from Lockheed Martin and from JPL, a
division of the California Institute of Technology in Pasadena.

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MRO HiRISE Images - October 8, 2008

MARS RECONNAISSANCE ORBITER HIRISE IMAGES
October 8, 2008

o Stratigraphy Exposed in Ius Chasma
http://hirise.lpl.arizona.edu/PSP_007430_1725

o Eroded Sediments in West Candor Chasma
http://hirise.lpl.arizona.edu/PSP_009460_1745

o Double Impact Crater
http://hirise.lpl.arizona.edu/PSP_009619_1630

o Saltating Gypsum into Dark Polar Dunes
http://hirise.lpl.arizona.edu/PSP_009656_2780


All of the HiRISE images are archived here:

http://hirise.lpl.arizona.edu/

Information about the Mars Reconnaissance Orbiter is online at
http://www.nasa.gov/mro. The mission is managed by NASA's Jet Propulsion
Laboratory, a division of the California Institute of Technology, for the NASA
Science Mission Directorate, Washington, D.C. Lockheed Martin Space Systems,
of Denver, is the prime contractor and built the spacecraft. HiRISE is operated by t
he University of Arizona. Ball Aerospace and Technologies Corp., of Boulder, Colo.,
built the HiRISE instrument.

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Thursday, October 9, 2008

NASA's Mars Odyssey Shifting Orbit for Extended Mission

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

Guy Webster 818-354-6278
Jet Propulsion Laboratory, Pasadena, Calif.
guy.webster@jpl.nasa.gov

Dwayne Brown 202-358-1726
Headquarters, Washington
dwayne.c.brown@nasa.gov

NEWS RELEASE: 2008-191 October 9, 2008

NASA's Mars Odyssey Shifting Orbit for Extended Mission

PASADENA, Calif. -- The longest-serving of six spacecraft now studying Mars is up to new tricks
for a third two-year extension of its mission to examine the most Earthlike of known foreign planets.

NASA's Mars Odyssey is altering its orbit to gain even better sensitivity for its infrared mapping of
Martian minerals. During the mission extension through September 2010, it will also point its camera
with more flexibility than it has ever used before. Odyssey reached Mars in 2001.

The orbit adjustment will allow Odyssey's Thermal Emission Imaging System to look down at sites
when it's mid-afternoon, rather than late afternoon. The multipurpose camera will take advantage of
the infrared radiation emitted by the warmer rocks to provide clues to the rocks' identities.

"This will allow us to do much more sensitive detection and mapping of minerals," said Odyssey
Project Scientist Jeffrey Plaut of NASA's Jet Propulsion Laboratory, Pasadena, Calif.

The mission's orbit design before now used a compromise between what works best for the Thermal
Emission Imaging System and what works best for another instrument, the Gamma Ray
Spectrometer.

On commands from its operations team at JPL and at Denver-based Lockheed Martin Space Systems,
Odyssey fired thrusters for nearly 6 minutes on Sept. 30, the final day of the mission's second two-
year extension.

"This was our biggest maneuver since 2002, and it went well," said JPL's Gaylon McSmith, Odyssey
mission manager. "The spacecraft is in good health. The propellant supply is adequate for operating
through at least 2015."

Odyssey's orbit is synchronized with the sun. The local solar time has been about 5 p.m. at whatever
spot on Mars Odyssey flew over as it made its dozen daily passes from between the north pole region
to the south pole region for the past five years. (Likewise, the local time has been about 5 a.m. under
the track of the spacecraft during the south-to-north leg of each orbit.)

The push imparted by the Sept. 30 maneuver will gradually change that synchronization over the next
year or so. Its effect is that the time of day on the ground when Odyssey is overhead is now getting
earlier by about 20 seconds per day. A follow-up maneuver, probably in late 2009 when the overpass
time is between 2:30 and 3:00 p.m., will end the progression toward earlier times.

While aiding performance of the Thermal Emission Imaging System, the shift to mid-afternoon is
expected to stop the use of one of three instruments in Odyssey's Gamma Ray Spectrometer suite.
The suite's gamma ray detector needs a later-hour orbit to avoid overheating of a critical component.
The suite's neutron spectrometer and high-energy neutron detector are expected to keep operating.

The Gamma Ray Spectrometer provided dramatic discoveries of water-ice near the surface
throughout much of high-latitude Mars, the impetus for NASA's Phoenix Mars Lander mission. The
gamma ray detector has also mapped global distribution of many elements, such as iron, silicon and
potassium, a high science priority for the first and second extensions of the Odyssey mission. A panel
of planetary scientists assembled by NASA recommended this year that Odyssey make the orbit
adjustment to get the best science return from the mission in coming years.

Increased sensitivity for identifying surface minerals is a key science goal for the mission extension
beginning this month. Also, the Odyssey team plans to begin occasionally aiming the camera away
from the straight-down pointing that has been used throughout the mission. This will allow the team
to fill in some gaps in earlier mapping and also create some stereo, three-dimensional imaging.

Odyssey will continue providing crucial support for Mars surface missions as well as conducting its
own investigations. It has relayed to Earth nearly all data returned from NASA rovers Spirit and
Opportunity. It shares with NASA's Mars Reconnaissance Orbiter the relay role for Phoenix. It has
made targeted observations for evaluating candidate landing sites.

Mars Odyssey, launched in 2001, is managed by JPL, a division of the California Institute of
Technology, Pasadena, for NASA's Science Mission Directorate, Washington. Lockheed Martin
Space Systems, Denver, is the prime contractor for the project and built the spacecraft. Investigators
at Arizona State University, Tempe, operate the Thermal Emission Imaging System. Investigators at
the University of Arizona, Tucson, head operation of the Gamma Ray Spectrometer. Additional
science partners are located at the Russian Aviation and Space Agency, which provided the high-
energy neutron detector, and at Los Alamos National Laboratories, New Mexico, which provided the
neutron spectrometer.

For more about the Mars Odyssey mission, visit: http://mars.jpl.nasa.gov/odyssey .

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NASA Maps Shed Light on Carbon Dioxide's Global Nature

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

Alan Buis 818-354-0474
Jet Propulsion Laboratory, Pasadena, Calif.
Alan.buis@jpl.nasa.gov

NEWS RELEASE: 2008-189 Oct. 9, 2008

NASA Maps Shed Light on Carbon Dioxide's Global Nature

PASADENA, Calif. --A NASA/university team has published the first global satellite maps of the
key greenhouse gas carbon dioxide in Earth's mid-troposphere, an area about 8 kilometers, or 5 miles,
above Earth. The team's study reveals new information on how carbon dioxide, which directly
contributes to climate change, is distributed in Earth's atmosphere and moves around our world.

A research team led by Moustafa Chahine of NASA's Jet Propulsion Laboratory, Pasadena, Calif.,
found the distribution of carbon dioxide in the mid-troposphere is strongly influenced by major
surface sources of carbon dioxide and by large-scale atmospheric circulation patterns, such as the jet
streams and weather systems in Earth's mid-latitudes. Patterns of carbon dioxide distribution were
also found to differ significantly between the northern hemisphere, with its many land masses, and
the southern hemisphere, which is largely covered by ocean.

The findings are based on data collected from the Atmospheric Infrared Sounder (AIRS) instrument
on NASA's Aqua spacecraft between September 2002 and July 2008. Chahine, the instrument's
science team leader, said the research products will be used by scientists to refine models of the
processes that transport carbon dioxide within Earth's atmosphere.

"These data capture global variations in the distribution of carbon dioxide over time," Chahine said.
"These variations are not represented in the four chemistry-transport models used to determine where
carbon dioxide is created and stored."

Chahine said the AIRS data will complement existing and planned ground and aircraft measurements
of carbon dioxide, as well as upcoming satellite missions to study Earth's carbon cycle and climate.
Included in the new satellite missions is NASA's Orbiting Carbon Observatory, planned for launch in
January 2009. The combination of carbon dioxide data from AIRS and the Orbiting Carbon
Observatory will allow scientists to determine the distribution of carbon dioxide in the lower
atmosphere, above Earth's surface.

"Carbon dioxide is difficult to measure and track," he said. "No place on Earth is immune from its
influence. It will take many independent measurements, including AIRS, to coax this culprit out of
hiding and track its progress from creation to storage."

The new maps reveal enhanced concentrations of carbon dioxide south of the northern hemisphere jet
stream, in a band between 30 and 40 degrees north latitude. These enhanced concentrations
correspond to a well-documented belt of pollution in the northern hemisphere mid-latitudes.

The team attributed the increased levels of carbon dioxide detected over the western North Atlantic to
emissions transported from the Southeast U.S. on warm atmospheric "conveyor belts." These belts
lift carbon dioxide from Earth's surface into the middle and upper troposphere. The AIRS maps also
showed enhanced carbon dioxide over the Mediterranean, resulting from North American and
European sources. Carbon dioxide from South Asia ended up over the Middle East, while carbon
dioxide from East Asia flowed out over the Pacific Ocean.

In the southern hemisphere, a belt of mid-tropospheric air containing enhanced concentrations of
carbon dioxide emerged between 30 and 40 degrees south latitude. This belt had not previously been
seen in the four chemistry-transport models used in this study. The researchers say the flow of air in
this belt over South America's high Andes Mountains lifts carbon dioxide from major sources on
Earth's surface, such as the respiration of plants, as well as forest fires and facilities used for synthetic
fuel production and power generation. A portion of this lifted carbon dioxide is then carried into the
mid-troposphere, where it becomes trapped in the mid-latitude jet stream and transported rapidly
around the world. "The troposphere is like international waters," Chahine said. "What's produced in
one place will travel elsewhere."

Study results were published recently in Geophysical Research Letters. Other participants included
the California Institute of Technology, Pasadena, Calif.; and the University of California, Irvine.

More information on AIRS is online at http://airs.jpl.nasa.gov/ .

JPL is managed for NASA by Caltech.

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Wednesday, October 8, 2008

Splashy Portrait Helps Explain How Stars Form

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

Whitney Clavin 818-354-4673
Jet Propulsion Laboratory
whitney.clavin@jpl.nasa.gov

Image Advisory: 2008-188 Oct. 8, 2008

Splashy Portrait Helps Explain How Stars Form

Different wavelengths of light swirl together like watercolors in a new, ethereal portrait of a
bright, star-forming region.

The multi-wavelength picture combines infrared, visible and X-ray light from NASA's Spitzer
Space Telescope, the European Southern Observatory's New Technology Telescope, and the
European Space Agency's XMM-Newton orbiting X-Ray telescope, respectively.

The colorful image offers a fresh look at the history of the star-studded region, called NGC
346, revealing new information about how stars form in the universe. NGC 346 is the brightest
star-forming region in the Small Magellanic Cloud, a so-called irregular dwarf galaxy that orbits
our Milky Way galaxy, 210,000 light-years away.

"NGC 346 is an astronomical zoo," said Dimitrios Gouliermis of the Max Planck Institute for
Astronomy in Germany, lead author of a new paper describing the observations in an upcoming
issue of the Astrophysical Journal. "When we combined data at various wavelengths, we were
able to tease apart what's going on in different parts of the cloud."

The new picture is available online at:
http://www.nasa.gov/mission_pages/spitzer/multimedia/20081008.html .

Small stars are scattered throughout the NGC 346 region, while massive stars populate its
center. The massive stars and most of the small stars formed at the same time out of one dense
cloud, while other small stars were created later through a process called triggered star
formation. Intense radiation from massive stars ate away at the surrounding dusty cloud,
triggering gas to expand and create shock waves that compressed nearby cold dust and gas into
new stars. The red-orange filaments surrounding the center of the image show where this
process has occurred.

But a set of even younger small stars in the region, seen as a pinkish blob at the top of the
image, couldn't be explained by this mechanism. Scientists were scratching their heads over
what caused this seemingly isolated group of stars to form.

By combining multi-wavelength data of NGC 346, Gouliermis says he and his team were able
to pinpoint the trigger as a very massive star that blasted apart in a supernova explosion about
50,000 years ago. According to the astronomers, this very massive star spurred the isolated
young stars into existence before it died, but through a different type of triggered star formation
than that which occurred near the center of the region. Fierce winds from the massive star, and
not radiation, pushed dust and gas together, compressing it into new stars.

The finding demonstrates that both wind- and radiation-induced triggered star formation are at
play in the same cloud. According to Gouliermis, "The result shows us that star formation is a far
more complicated process than we used to believe, comprising different competitive or
collaborative mechanisms."

The new image also reveals a bubble, seen as a blue halo to the left, caused by the supernova
explosion that happened 50,000 years ago. Further analysis shows that this bubble is located
within a large expanding gaseous shell, possibly powered by the explosion and the winds of
other bright stars in its vicinity.

Infrared light (red) shows cold dust; visible light (green) denotes glowing gas; and X-rays (blue)
represent very warm gas. Ordinary stars appear as blue spots with white centers, while young
stars enshrouded in dust appear as red spots with white centers.

Other authors of this paper include Thomas Henning and Wolfgang Brandner of the Max Planck
Institute for Astronomy, and You-Hua Chu and Robert Gruendl of the University of Illinois at
Urbana-Champaign.

NASA's Jet Propulsion Laboratory, Pasadena, Calif., manages the Spitzer Space Telescope
mission for NASA's Science Mission Directorate, Washington. Science operations are
conducted at the Spitzer Science Center at the California Institute of Technology, also in
Pasadena. Caltech manages JPL for NASA.

More information about Spitzer is at http://www.spitzer.caltech.edu/spitzer and
http://www.nasa.gov/spitzer .

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Tuesday, October 7, 2008

Artists and Astronomers 'Observe' the Universe Together

Feature October 7, 2008


Artists and Astronomers 'Observe' the Universe Together

Our current view of the universe, to quote Albert Einstein, is "not weirder than we do
imagine, but weirder than we can imagine." That said, we have no choice but to observe
the universe through human eyes and brains. How can we even start to make sense of it?

One answer might be to call in the artists. For thousands of years, people have used art to
explore ideas that humble, confuse or even frighten us. A new exhibition opening in
Pasadena continues this tradition, bringing artists and astronomers together to create
original pieces of art.

Called "Observe," the exhibition is the culmination of a yearlong collaboration between
two Pasadena institutions -- the Art Center College of Design and NASA's Spitzer
Science Center at the California Institute of Technology. Beginning Oct. 10, visitors to
the Art Center's Williamson Gallery will be challenged to stretch their imaginations as
infrared observations from NASA's Spitzer Space Telescope are visualized through the
minds of five contemporary Southern California artists.

"Science is bringing us spectacular discoveries that torque our everyday perception of
reality. Things like black holes, multiple universes and time distortions challenge our
human-centered culture and beliefs," said Stephen Nowlin, director of the Williamson
Gallery. "This is an exhibition about the newly unknown."

Dan Goods, an Observe artist and a visual strategist at NASA's Jet Propulsion Laboratory
in Pasadena, was fascinated by the idea that light from distant stars and galaxies travels
for years before reaching us. "Some of those stars died thousands of years ago, and they
only exist in the light that is still on its way to our eyes," he pointed out.

Goods built a clock that spans a large room. Spheres throughout the room represent the
hours. The spheres all look the same at the entrance, but like stars in the sky, they are
actually different sizes and distances away. Speakers on the spheres play back sounds
from people in the room, distorted and delayed by random time increments. This
distortion represents a phenomenon called "redshift" in astronomy, in which light is
stretched to longer wavelengths as it travels through space. "It's like the stars are talking
to you," Goods explained.

Other projects include an interactive video installation by Daniel Wheeler, which invites
visitors to "send" data all over the world to create an abstract collage of images; and a
planetarium-like room filled with changing projections of the stars by Lita Albuquerque.
George Legrady used a projected laser to make patterns representing all the pointing
commands that have been sent up to Spitzer in space. And Lynn Aldrich created a fake-
fur wormhole -- a theoretical tunnel through space and time -- that people can crawl
through.

"I was amazed by the serendipities that cropped up," said Michelle Thaller, outreach
manager at the Spitzer Science Center. "Lynn Aldrich's furry wormhole is a great way to
represent the weird, almost chaotic nature of other dimensions!"

"I've always thought that Spitzer's images were spectacular, but working with the artists
has made me look at scientific data in a whole new way," she added. "Data out of context
can become art."

Observe opens to the public on Oct. 10 as part of ArtNight Pasadena, a weekend of art
around town sponsored by the Pasadena Arts and Culture Commission. Opening-night
hours are 6 to 10 p.m. The exhibition will run though Jan. 9, 2009, ushering in the
International Year of Astronomy, a yearlong celebration of the 400th anniversary of
Galileo and the first telescope.

JPL manages the Spitzer mission for NASA's Science Mission Directorate, Washington.
Science operations are conducted at the Spitzer Science Center. Caltech manages JPL for
NASA.

More information about Spitzer is at www.spitzer.caltech.edu . More information about
the Art Center College of Design is at www.artcenter.edu . More information about
Pasadena ArtNight is at www.artcenter.edu/artnight .



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Monday, October 6, 2008

Small Asteroid to Light Up Sky Over Africa

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

DC Agle 818-393-9011
Jet Propulsion Laboratory, Pasadena, Ca.
agle@jpl.nasa.gov

Dwayne Brown 202-358-1726
NASA Headquarters, Washington
dwayne.c.brown@nasa.gov

NEWS RELEASE: 2008-186 Oct. 6, 2008

Small Asteroid to Light Up Sky Over Africa

WASHINGTON -- An asteroid measuring several feet in diameter is expected to enter the
atmosphere over northern Sudan before dawn Tuesday, setting off a potentially brilliant natural
fireworks display.

It is unlikely any sizable fragments will survive the fiery passage through Earth's atmosphere. The
event is expected to occur at 5:46 a.m. local time (10:46 p.m. EDT Monday).

"We estimate objects this size enter Earth's atmosphere once every few months," said Don Yeomans
of the Near-Earth Object Office at NASA's Jet Propulsion Laboratory in Pasadena, Calif. "The unique
aspect of this event is that it is the first time we have observed an impacting object during its final
approach."

The small space rock, designated 2008 TC3, will be traveling on an eastward trajectory that will carry
it toward the Red Sea.

"Observers in the region could be in for quite a show," Yeomans said. "When the object enters the
atmosphere, it could become an extremely bright fireball."

The small space rock first was observed by the Mount Lemmon telescope of the NASA-funded
Catalina Sky Survey early Monday and reported to the Minor Planet Center for initial orbit
determination. The Minor Planet Center alerted NASA and JPL of the impact potential. NASA
detects and tracks asteroids and comets passing close to Earth. The Near Earth Object Observation
Program, commonly called "Spaceguard," plots the orbits of these objects to determine if any could
be potentially hazardous to our planet.

For more information, visit: http://neo.jpl.nasa.gov/

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Cassini Plans Doubleheader Flybys of Saturn's Geyser Moon

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

Carolina Martinez 818-354-9382
Jet Propulsion Laboratory, Pasadena, Calif.
carolina.martinez@jpl.nasa.gov

NEWS RELEASE: 2008-185 Oct. 6, 2008

Cassini Plans Doubleheader Flybys of Saturn's Geyser Moon

PASADENA, Calif. -- As major league baseball readies for the World Series, NASA's Cassini
team will come to bat twice this month when the spacecraft flies by Saturn's geyser moon,
Enceladus.

The Oct. 9 flyby is an inside pitch—the closest flyby yet of any moon of Saturn, at only 25
kilometers (16 miles) from the surface. The Oct. 31 flyby is farther out, at 196 kilometers (122
miles).

Scientists are intrigued by the possibility that liquid water, perhaps even an ocean, may exist
beneath the surface of Enceladus. Trace amounts of organics have also been detected, raising
tantalizing possibilities about the moon's habitability.

While Cassini's cameras and other optical instruments were the focus of an Aug. 11 flyby, during
Cassini's Oct. 9 flyby, the spacecraft's fields and particles instruments will venture deeper into
the plume than ever before, directly sampling the particles and gases. The emphasis here is on
the composition of the plume rather than imaging the surface.

"We know that Enceladus produces a few hundred kilograms per second of gas and dust and that
this material is mainly water vapor and water ice," said Tamas Gambosi, Cassini scientist at the
University of Michigan, Ann Arbor. "The water vapor and the evaporation from the ice grains
contribute most of the mass found in Saturn's magnetosphere.

"One of the overarching scientific puzzles we are trying to understand is what happens to the gas
and dust released from Enceladus, including how some of the gas is transformed to ionized
plasma and is disseminated throughout the magnetosphere," said Gambosi.

On Oct. 31, the cameras and other optical remote sensing instruments will be front and center,
imaging the fractures that slash across the moon's south polar region like stripes on a tiger.


These two flybys might augment findings from the most recent Enceladus flyby, which hint at
possible changes associated with the icy moon. Cassini's Aug. 11 encounter with Enceladus
showed temperatures over one of the tiger-stripe fractures were lower than those measured in
earlier flybys. The fracture, called Damascus Sulcus, was about 160 to 167 Kelvin (minus 171 to
minus 159 degrees Fahrenheit), below the 180 Kelvin (minus 136 degrees Fahrenheit) reported
from a flyby in March of this year.

"We don't know yet if this is due to a real cooling of this tiger stripe, or to the fact that we were
looking much closer, at a relatively small area, and might have missed the warmest spot," said
John Spencer, Cassini scientist on the composite infrared spectrometer, at the Southwest
Research Institute, Boulder, Colo.

Results from Cassini's magnetometer instrument during the August flyby suggest a difference in
the intensity of the plume compared to earlier encounters. Information from the next two flybys
will help scientists understand these observations.

Four more Enceladus flybys are planned in the next two years, bringing the total number to
seven during Cassini's extended mission, called the Cassini Equinox Mission. The next
Enceladus doubleheader will be November 2 and 21, 2009.

The Enceladus geysers were discovered by Cassini in 2005. Since then, scientists have been
intrigued about what powers them, because the moon is so tiny, roughly the width of Arizona at
only 500 kilometers (310 miles) in diameter.

"The October doubleheader gives Cassini two more opportunities to hit the ball out of the park,"
said Bob Pappalardo, Cassini project scientist at NASA's Jet Propulsion Laboratory, Pasadena,
Calif. "With high scores in geology, surface heat, watery plumes and magnetospheric effects,
Enceladus could win the 'world championship' title this year!"

Scientists anticipate reporting results from the two flybys in November and early December.

Cassini has been orbiting Saturn since 2004. The Cassini-Huygens mission is a cooperative
project of NASA, the European Space Agency and the Italian Space Agency. JPL manages the
Cassini-Huygens mission for NASA's Science Mission Directorate. The Cassini orbiter was
designed, developed and assembled at JPL.

For images, videos and a mission blog on the flyby, visit: http://www.nasa.gov/cassini .
More information on the Cassini mission is also available at http://saturn.jpl.nasa.gov .

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