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Thursday, January 31, 2008

Cassini Finds Rhythm in Saturn's Rings

Feature January 31, 2008



Cassini Finds Rhythm in Saturn's Rings

Order can be found in the most unexpected places, as demonstrated
by our neighbor three planets down. Two of Saturn's rings have
been found by NASA's Cassini spacecraft to contain orderly lines
of densely grouped, boulder-size icy particles that extend outward
across the rings like ripples from a rock dropped in a calm pond.

"Imagine going to a town that stretches from San Francisco to Los
Angeles and seeing buildings spaced the same distance apart on
every block," said Cassini radio science team member Essam
Marouf of San Jose State University, San Jose, Calif. "All of these
groups of particles within the rings are very close together, and the
space between them is extremely small, only 100 to 250 meters
(320 feet to 820 feet) wide, depending on where they are in the
ring."

Normally, the distances between particles change with their
velocity. In the case of Saturn's rings, the distances between these
ring particles stay relatively equal even though their velocities may
change. This type of pattern is completely new, according to
Marouf.

"This particular feature is the smallest and most detailed of
anything seen in Saturn's rings so far," Marouf said. "In the
chaotic environment of the rings, to find such regularity in the
most cramped areas is nothing short of amazing." The regular
structure can only be found in locations where particles are densely
packed together, such as the B ring and the innermost part of the A
ring.

The unexpected pattern within Saturn's rings may give scientists
some new ideas of what to expect from other similar planets and
solar systems.

The pattern was detected when the radio on board the Cassini
spacecraft sent out three signals toward Earth. The signals crossed
the Saturn's rings, and their frequencies were separated by
scattering from the ring particles. Once the signals were captured
by Earth-based antennas of NASA's Deep Space Network, Cassini
scientists saw a regular pattern in the received signal frequencies.

"The signals showed that the particle groups were arranged in an
unexpectedly regular formation that had 'rhythm within the rings of
Saturn,'" said Marouf. "Each particle is in its own orbit, and
sometimes they collide and move apart as their velocities change.
As a result, you have particles bunched together into dense groups
that extend across the ring in harmony with each other."

The pattern of particles is described as an enormously extended
natural diffraction grating. A diffraction grating has parallel lines
like a picket fence; when light hits this fence, it separates
according to wavelength, from ultraviolet to infrared light.

The same thing happened when Cassini's radio signals hit the
fencelike pattern of ring particles. The signals, sent out in 2005,
were meant to capture a complete view of the rings.

This research appears as a cover story in the Dec. 28 issue of
Geophysical Research Letters.

Written by: Diya Chacko
Media Relations Contact: Carolina Martinez 818-354-9382

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NASA and the Beatles Celebrate Anniversaries by Beaming Song 'Across the Universe' Into Deep Space

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

Michael Cabbage 202-358-1600
Headquarters, Washington
mcabbage@nasa.gov

Veronica McGregor 818-354-5011
Jet Propulsion Laboratory, Pasadena, Ca.
veronica.mcgregor@jpl.nasa.gov

Martin Lewis 323-972-7755
Springtime!
martin@martinlewis.com

NEWS RELEASE 2008-019 Jan. 31, 2008

NASA and the Beatles Celebrate Anniversaries by Beaming Song 'Across the
Universe' Into Deep Space

WASHINGTON – For the first time ever, NASA will beam a song – The Beatles "Across
the Universe" -- directly into deep space at 4 p.m. Pacific Time (7 p.m. Eastern Time) on
Monday, Feb. 4.

The transmission over NASA's Deep Space Network will commemorate the 40th
anniversary of the day The Beatles recorded the song, as well as the 50th anniversary of
NASA's founding and the group's beginnings. Two other anniversaries also are being
honored: The launch 50 years ago this week of Explorer 1, the first U.S. satellite, and the
founding 45 years ago of the Deep Space Network, an international network of antennas
that supports missions to explore the universe.

Technicians at NASA's Jet Propulsion Laboratory, Pasadena, Calif., where the Deep
Space Network is managed, will send the command that will start the transmission.

The transmission is being aimed at the North Star, Polaris, which is located 431 light
years away from Earth. The song will travel across the universe at a speed of 186,000
miles per second. Former Beatle Sir Paul McCartney expressed excitement that the tune,
which was principally written by fellow Beatle John Lennon, was being beamed into the
cosmos.

"Amazing! Well done, NASA!" McCartney said in a message to the space agency. "Send
my love to the aliens. All the best, Paul."

Lennon's widow, Yoko Ono, characterized the song's transmission as a significant event.

"I see that this is the beginning of the new age in which we will communicate with
billions of planets across the universe," she said.

It is not the first time Beatles music has been used by NASA; in November 2005,
McCartney performed the song "Good Day Sunshine" during a concert that was
transmitted to the International Space Station. "Here Comes the Sun," "Ticket to Ride"
and "A Hard Day's Night" are among other Beatles' songs that have been played to wake
astronaut crews in orbit.

Feb. 4 has been declared "Across The Universe Day" by Beatles fans to commemorate
the anniversaries. As part of the celebration, the public around the world has been invited
to participate in the event by simultaneously playing the song at the same time it is
transmitted by NASA. Many of the senior NASA scientists and engineers involved in the
effort are among the group's biggest fans.

"I've been a Beatles fan for 45 years – as long as the Deep Space Network has been
around," said Barry Geldzahler, the network's program executive at NASA Headquarters,
Washington. "What a joy, especially considering that 'Across the Universe' is my
personal favorite Beatles song."

JPL built the Explorer 1 satellite and is celebrating the 50th anniversary of its launch. JPL
also operates NASA's Deep Space Network. For information about the Deep Space
Network, go to:

http://deepspace.jpl.nasa.gov

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Journey to Saturn From Your Computer

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/Diya Chacko 818-354-9382/818-393-5464
Jet Propulsion Laboratory, Pasadena, Calif.
carolina.martinez@jpl.nasa.gov/dschacko@jpl.nasa.gov

INTERNET ADVISORY: 2008-018 Jan. 31, 2008

Journey to Saturn From Your Computer

Want a peek at Saturn as seen from space? A new interactive 3-D viewer that uses a
game engine and allows users to travel to Saturn and see it the way the Cassini spacecraft
sees it is now online at http://saturn.jpl.nasa.gov/multimedia/CASSIE and
http://www.nasa.gov/mission_pages/cassini/multimedia/cassie.html .

The Cassini at Saturn Interactive Explorer makes the real Cassini mission data fully
available in three colorful, easy-to-use expeditions.

The "Where is Cassini Now?" expedition shows exactly where the Cassini spacecraft is
and what it is doing each moment over the current 24-hour period. Viewers can see the
spacecraft move in its orbit and maneuver according to instructions from mission
scientists and navigators at NASA's Jet Propulsion Laboratory, Pasadena, Calif.

With the "Mission Overview" expedition, look back in time as Cassini orbited the Saturn
system over the past 3.5 years, and fast-forward into the future to see where it is headed.
Users can control two virtual cameras to see Cassini fly by Saturn and its moons.

The "Saturn's Moons" expedition gives an in-depth peek at seven of Saturn's moons,
providing useful facts and interactive surface views of each one.

More information on the Cassini mission is available at http://www.nasa.gov/cassini and

http://saturn.jpl.nasa.gov .

The Cassini-Huygens mission is a cooperative project of NASA, the European Space
Agency and the Italian Space Agency. JPL, a division of the California Institute of
Technology in Pasadena, manages the Cassini-Huygens mission for NASA's Science
Mission Directorate, Washington. The Cassini orbiter was designed, developed and
assembled at JPL.
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NASA Finds Glacial Sediments Adding to Louisiana Coast's Sinking

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: 2008-017 Jan. 31, 2008

NASA Finds Glacial Sediments Adding to Louisiana Coast's Sinking

PASADENA, Calif. – A study by NASA and Louisiana State University scientists finds that
sediments deposited into the Mississippi River Delta thousands of years ago when North
America's glaciers retreated are contributing to the ongoing sinking of Louisiana's coastline. The
weight of these sediments is causing a large section of Earth's crust to sag at a rate of 0.1 to 0.8
centimeters (0.04 to 0.3 inches) a year.

The sediments pose a particular challenge for New Orleans, causing it to sink irreversibly at a
rate of about 0.4 centimeters (0.17 inches) a year, according to data from a network of global
positioning system stations and a model of sediment data collected from the northern Gulf of
Mexico and the Mississippi Delta.

Hurricanes Katrina and Rita in 2005 focused national attention on the Gulf coast's vulnerability
to hurricanes due to loss of wetlands and sea level rise. These new findings add another factor for
scientists, government agencies and the public to consider when assessing the vulnerability of the
region to hurricanes and large storms.

A science team led by Erik Ivins of NASA's Jet Propulsion Laboratory, Pasadena, Calif.,
hypothesized that Earth's very slow gravitational flow response to the weight of the sediments,
combined with a 130-meter (427-foot) rise in sea level that took place thousands of years ago, are
contributing to the sinking of a 199,000-square kilometer (77,000-square-mile) section of coastal
Louisiana.

To test their theory, the team developed a physical model of sinking caused by both the weight of
the sea level rise and the flow of glacial sediments into the Gulf of Mexico following the retreat
of the great ice sheet that covered much of North America some 22,000 years ago. The model
spanned the past 750,000 years. Results were compared with actual global positioning system
measurements and other geophysical data for southern Louisiana and the Gulf, collected from
multiple sources over the past 60 years.

The scientists found the model results were in good agreement with the actual geophysical data,
predicting sinking of between 0.1 centimeters (0.04 inches) and 0.8 centimeters (0.3 inches) a
year. The highest sinking rates were observed where coastal land loss is greatest, near the center
of the Mississippi and Atchafalaya River Delta complexes.

"Our study shows that the weight of these sediments on Earth's crust can explain between 0.1 and
0.8 centimeters (0.04 and 0.3 inches) of sinking per year," said study co-author Roy Dokka of
Louisiana State University, Baton Rouge. "These sediments contribute a part of the region's
sinking that's inevitable and must be considered when predicting rates of sinking and future sea
level change in coastal Louisiana."

The scientists say when these results are combined with sinking totaling about 0.3 centimeters
(0.12 inches) per year caused by other factors such as compaction and oxidation of sediments,
pumping of oil and water by humans, faulting and sea level rise, the overall outlook isn't bright.
"Louisiana is slowly losing its battle with the Gulf of Mexico," said Ivins. "Our model predicts
this rate of sinking will continue for hundreds of years. Continued sinking, along with the
sediment starvation of the coast caused by construction of flood control levees along the
Mississippi River, will ultimately lead to the drowning of the coast."

Co-author Ron Blom of JPL adds that New Orleans is particularly vulnerable. "When the effect
of this sinking near New Orleans is combined with a potential 0.9 centimeter (0.35 inch) annual
sea level rise that could result should ice sheet melting accelerate as projected by many climate
models, it is possible New Orleans could see a relative sea level rise of roughly one meter (3.3
feet) in the next 90 years," Blom said.

The good news, the authors say, is that, with refinement, their model may help the region prepare
better for future large storms and the gradual inundation of the coast. "Our model gives civil
engineers and disaster preparedness managers very precise predictions of how the landscape is
changing so that they can better mitigate the effects of this sinking," said Ivins. "Understanding
all of the processes affecting the coast is essential for engineering effective solutions."

Louisiana's coast is far from the centers of North America's former ice sheets, which were once
as large as Antarctica, but successive periods of glacier formation and retreat have affected the
region through sea level rises and changes in the flow of glacial sediments into the Gulf of
Mexico. This process has been ongoing in cycles caused by regular variations in Earth's orbit.
When the glaciers retreated, the resulting flooding transported large volumes of sediments down
today's major river systems -- three to four times more than the Mississippi River currently
transports.

The authors say the relative fluidity of Earth's upper mantle beneath the Gulf coast is the primary
factor that determines how Earth's crust responds to deposited sediments. Earth's crust and
uppermost mantle is weaker beneath the Gulf of Mexico than it is beneath eastern Canada.

Results of the study are published in Geophysical Research Letters. The research was funded by
NASA, the National Science Foundation and the Louisiana Board of Regents.

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

Additional media contact for this story: Ernie Ballard, Louisiana State University, 225-578-5685,
eballa1@lsu.edu .

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

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First Light Newsletter - January 2008

First Light eNewsletter
January 2008



Explorer 1: America's First Spacecraft

On Jan. 31, 1958, the JPL-designed and -built Explorer 1 soared into space. The spacecraft, a quick response to the Soviet's Sputnik, lofted the United States into the Space Age.

Visit JPL's Explorer 1 site to learn about the historic event, watch archival video footage, and take an interactive peek inside the satellite.
http://www.jpl.nasa.gov/explorer (http://www.jpl.nasa.gov/explorer)



Explorer 1: Beginning of the Space Age Debuts Jan. 31, 6 p.m. (Pacific)

(Click the events link (http://www.jpl.nasa.gov/explorer/media/info.php) for more viewing times on Discovery HD Theater and KCET/Los Angeles.)


Now Playing on the JPL Web


Keeping an Eye on Space Rocks

Asteroids swinging near Earth and Mars have been in the news recently. Animations and interactive features help explain what near-Earth objects are, and why scientists track them.
+ Go to interactive (http://www.jpl.nasa.gov/multimedia/neo/index.cfm)


The Challenges of Getting to Mars: Cruise Phases
The next mission to Mars is fast-approaching the red planet. Phoenix is scheduled to land in the north polar
region of Mars in May. A new video shows how the mission team is keeping Phoenix on its path for the eight-month journey.
+ Play video (http://www.jpl.nasa.gov/videos/phoenix/phx20080124/)

Explore New Worlds Virtually
How are scientists searching for planets beyond our solar system? The PlanetQuest site , sporting a newlook, offers in-depth information, interactives and
an online New Worlds Atlas. You can also download toa widget to keep up with current planet count.
+ Visit PlanetQuest (http://planetquest.jpl.nasa.gov/)

You can find more features at www.jpl.nasa.gov (http://www.jpl.nasa.gov)



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Gardens on Mars - "Designing for the First Community on Mars"

Gardens on Mars - "Designing for the First Community on Mars"

Where's a cool place to hang if you're an explorer on Mars? A new class will
encourage high school students to let their artistry and imagination loose as they
envision a futuristic community on the Red Planet. The class, for students in
grades 9 through 12, is sponsored by JPL, the Art Center College of Design,
Pasadena and the Huntington Library and Botanical Gardens.

Classes will be held Saturdays at the Art Center from 9 a.m. to 1 p.m, Feb. 2 –
Apr. 12 (Holiday: Apr. 7). Late enrollment ends Feb. 8. The cost of the class is
$300; estimated cost of materials is $45.

Student teams will be challenged to imagine the first human community on Mars
and to think creatively about ways to create a cool "hangout" for our first Martian
explorers. Sketching, illustration and modelmaking instruction will be provided.

Students will work directly with artists, designers and NASA scientists in the
creation of their ideas. Tours of JPL and the Huntington will be included.

For information contact: David Delgado, JPL, david.j.delgado@jpl.nasa.gov
(818) 393-5144. This is an Imagine Mars project: http://imaginemars.jpl.nasa.gov

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Monday, January 28, 2008

Linked Hawaiian Telescopes Catch a Nova Surprise

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


Jane Platt 818-354-0880
Jet Propulsion Laboratory, Pasadena, Calif.
Jane.platt@jpl.nasa.gov

NEWS RELEASE: 2008-016 Jan. 28, 2008

Linked Hawaiian Telescopes Catch a Nova Surprise

First results from a new NASA-funded scientific instrument at the W. M. Keck Observatory
at Mauna Kea, Hawaii, are helping scientists overturn long-standing assumptions about
powerful explosions called novae and have produced specific information about one nearby
nova.

This sophisticated new system, called the Keck Interferometer, combines the observing power
of the two 10-meter (33 feet) Keck telescopes into a single mega-telescope. Using the
interferometer's "nulling" mode, data were taken by the Keck Interferometer team on a nearby
nova called RS Ophiuchi.

In "nulling" mode, the Keck Interferometer suppresses the blinding light of a star so
researchers can study the surrounding environment. The instrument helps them observe very
faint objects near bright sources and produces 10 times more resolving power than a single
Keck telescope working alone. It is the only instrument of its kind in operation.

The nulling mode was developed to search for dust regions around nearby stars, where planets
might be forming, but the bright starlight poses a great challenge. "Because a star is so much
brighter than the dust, something has to block the light, which is what the nuller does," said
Rachel L. Akeson, Keck Interferometer project scientist at the California Institute of
Technology's Michelson Science Center. "This technique turns out to be useful for lots of
other kinds of objects, including this one, where dust is near a star that just went nova."

These nova data were taken by a team led by Wes Traub of NASA's Jet Propulsion
Laboratory, Pasadena, Calif., and the data analysis and unified model for the nova were
produced by a team led by Richard Barry and William Danchi of the Goddard Space Flight
Center, Greenbelt, Md.

The star in the constellation Ophiuchus went nova at the perfect time for the team, on Feb. 12,
2006. "We were extremely lucky, because we had astronomers in place at two mountain-top
interferometers, Keck in Hawaii and Infrared Optical Telescope Array in Arizona. Within
minutes of hearing about the discovery of the nova, we alerted both teams to start observing it
that night," said Traub, a senior research scientist at JPL.

The nova system, known as RS Oph consists of a white dwarf and a red giant. The red giant is
gradually shedding its massive gaseous outer layers, and the white dwarf is sweeping up much
of this wind, growing in mass over time. As the matter builds up on the white dwarf's surface,
it eventually reaches a critical temperature that ignites a thermonuclear explosion that causes
the system to brighten 600-fold. RS Oph was previously observed blowing its stack in 1898,
1933, 1958, 1967 and 1985, so astronomers were eagerly anticipating the 2006 eruption.

About three-and-a-half days after the nova was detected, the group observed the explosion
with the Keck nuller. They set the instrument to cancel the nova's light, allowing them to see
the much fainter surrounding material, and then the extremely bright blast zone.

The instrument's versatility was key to a surprising discovery. The nuller saw no dust in the
bright zone, presumably because the nova's blast wave vaporized dust particles. But farther
from the white dwarf, at distances starting around 20 times the Earth-sun distance, the nuller
recorded the spectral chemical signature of silicate dust. The blast wave had not yet reached
this zone, so the dust must have pre-dated the explosion.

"This flies in the face of what we expected. Astronomers had previously thought that nova
explosions actually create dust," said Richard Barry of Goddard, lead author of the paper on
the observations that will appear in the Astrophysical Journal. The team thinks the dust is
created as the white dwarf plows through the red giant's wind, creating a pinwheel pattern of
higher-density regions that is reminiscent of galaxy spiral arms. Inside these arms, atoms
become cool enough and dense enough to allow atoms to stick together to form dust particles.
The nova's blast wave has since destroyed RS Oph's pinwheel pattern, but it should re-form
over the next few years, and future observations by NASA's Spitzer Space Telescope could
see it. Barry is also coauthor of a paper based on Spitzer observations of RS Oph.

Most studies of RS Oph have relied on spectroscopic models, which have not been able to
distinguish various nova components with as much detail as the interferometer. The Keck
nuller measured one component of the RS Oph system to an accuracy of just
4 milliarcseconds, or about the size of a basketball seen 7,500 miles away.

The Keck Interferometer is part of NASA's ongoing quest to search for planets orbiting other
stars. JPL, a division of Caltech, manages the Keck Interferometer for NASA. The Keck
Interferometer was developed by JPL, the W.M. Keck Observatory and the Michelson
Science Center. The W.M. Keck Observatory is funded by Caltech, the University of
California and NASA, and is managed by the California Association for Research in
Astronomy, Kamuela, Hawaii. More information on the Keck Interferometer is at

http://ki.jpl.nasa.gov .

Additional contact: Laura Kinoshita/Keck Observatory, Mauna Kea, Hawaii:
877-239-3067 laura@laura-kinoshita.com


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Friday, January 25, 2008

NASA Scientists Get First Images of Earth Flyby Asteroid

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

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

Grey Hautaluoma 202-358-0668
Headquarters, Washington
grey.hautaluoma-1@nasa.gov

NEWS RELEASE: 2008-014 Jan. 25, 2008

NASA Scientists Get First Images of Earth Flyby Asteroid

Scientists at NASA's Jet Propulsion Laboratory in Pasadena, Calif., have obtained the
first images of asteroid 2007 TU24 using high-resolution radar data. The data indicate the
asteroid is somewhat asymmetrical in shape, with a diameter roughly 250 meters (800
feet) in size. Asteroid 2007 TU24 will pass within 1.4 lunar distances, or 538,000
kilometers (334,000 miles), of Earth on Jan. 29 at 12:33 a.m. Pacific time (3:33
a.m. Eastern time).

"With these first radar observations finished, we can guarantee that next week's 1.4-lunar-
distance approach is the closest until at least the end of the next century," said Steve
Ostro, JPL astronomer and principal investigator for the project. "It is also the asteroid's
closest Earth approach for more than 2,000 years."

Scientists at NASA's Near-Earth Object Program Office at JPL have determined that
there is no possibility of an impact with Earth in the foreseeable future.

Asteroid 2007 TU24 was discovered by the NASA-sponsored Catalina Sky Survey on
Oct. 11, 2007. The first radar detection of the asteroid was acquired on Jan. 23 using the
Goldstone 70-meter (230-foot) antenna. The Goldstone antenna is part of NASA's Deep
Space Network Goldstone station in Southern California's Mojave Desert. Goldstone's
70-meter diameter (230-foot) antenna is capable of tracking a spacecraft traveling more
than 16 billion kilometers (10 billion miles) from Earth. The surface of the 70-meter
reflector must remain accurate within a fraction of the signal wavelength, meaning that
the precision across the 3,850-square-meter (41,400-square-foot) surface is maintained
within one centimeter (0.4 inch).

Ostro and his team plan further radar observations of asteroid 2007 TU24 using the
National Science Foundation's Arecibo Observatory in Puerto Rico on Jan. 27-28 and
Feb. 1-4.

The asteroid will reach an approximate apparent magnitude 10.3 on Jan. 29-30 before
quickly becoming fainter as it moves farther from Earth. On that night, the asteroid will
be observable in dark and clear skies through amateur telescopes with apertures of at least
7.6 centimeters (three inches). An object with a magnitude of 10.3 is about 50 times
fainter than an object just visible to the naked eye in a clear, dark sky.

Scientists working with Ostro on the project include Lance Benner and Jon Giorgini
of JPL, Mike Nolan of the Arecibo Observatory, and Greg Black of the University of
Virginia.

NASA detects and tracks asteroids and comets passing close to Earth. The Near Earth
Object Observation Program, commonly called "Spaceguard," discovers, characterizes
and computes trajectories for these objects to determine if any could be potentially
hazardous to our planet. The Arecibo Observatory is part of the National Astronomy
and Ionosphere Center, a national research center operated by Cornell University, Ithaca,
N.Y., for the National Science Foundation. JPL is a division of the California Institute of
Technology in Pasadena.

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

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Feature: Cosmic Suburbia is a Better Breeding Ground for Stars

Cosmic Suburbia is a Better Breeding Ground for Stars

New observations from NASA's Spitzer Space Telescope suggest that galaxies
prefer to raise stars in cosmic suburbia rather than in "big cities."

Galaxies across the universe reside in cosmic communities, big and small. Large,
densely populated galactic communities are called galaxy clusters. Like big cities
on Earth, galaxy clusters are scattered throughout the universe, connected by a
web of dusty "highways" called filaments. While thousands of galaxies live
within the limits of a cluster, smaller galactic communities are sprinkled along
filaments, creating celestial suburbs. Over time, astronomers suspect that all
galactic suburbanites will make their way to a cluster by way of filaments.

For the first time, Spitzer's supersensitive eyes have caught an infrared glimpse of
several galaxies traveling along two filamentary roads into a galaxy cluster called
Abell 1763.

"This is the first time we've ever seen a filament leading into a cluster with an
infrared telescope," says Dario Fadda, of the Herschel Science Center, which is
located at the California Institute of Technology in Pasadena, Calif.

"Our observations show that the fraction of starburst galaxies in the filaments is
more than double the number of starburst galaxies inside the cluster region," he
adds.

According to Fadda, clusters and the filaments that connect them are among the
largest structures in the cosmos. To see them, astronomers need instruments that
can map large areas of sky and have the sensitivity to resolve individual galaxies.

Luckily, instruments aboard Spitzer can do both. Using the telescope's multiband
imaging photometer, Fadda and his colleagues saw structures spanning 23 million
light-years. They used the observatory's infrared array camera to collect a census
of each galaxy's star formation and used a ground-based telescope at the Kitt Peak
National Observatory near Tucson, Ariz., to determine which galaxies belonged
to the cluster and surrounding filaments. Ultimately, Fadda found that galaxies in
the filaments form stars at a higher rate than their cluster counterparts.

"The new Spitzer findings will provide valuable insights into how galaxies grow
and change as they leave cosmic suburbia for the big cities," says Fadda.

He notes that future infrared missions will be able to follow in Spitzer's footsteps
and study how filaments and clusters affect the growth of galaxies in greater
detail. One such mission is the European Space Agency's Herschel Space
Telescope, which has significant NASA involvement.

His paper on this topic has been accepted for publication in Astrophysical Journal
Letters. Co-authors on the paper include Andrea Biviano of the
INAF/Osservatorio Astronomico di Trieste, Italy; Florence Durret of Institut
d'Astrophysique de Paris, France; and Francine Marleau and Lisa Storrie-
Lombardi of the Spitzer Science Center, Pasadena, Calif.

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.

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Mars Odyssey THEMIS Images: January 21-25, 2008

MARS ODYSSEY THEMIS IMAGES
January 21-25, 2008

o Aonia Terra Dunes (Released 21 January 2008)

http://themis.asu.edu/zoom-20080121a

o Copernicus Dunes (Released 22 January 2008)

http://themis.asu.edu/zoom-20080122a

o Dust Devil Tracks (Released 23 January 2008)

http://themis.asu.edu/zoom-20080123a

o Gullies (Released 24 January 2008)

http://themis.asu.edu/zoom-20080124a

o Gullies (Released 25 January 2008)

http://themis.asu.edu/zoom-20080125a


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 - January 24, 2008

MARS RECONNAISSANCE ORBITER HIRISE IMAGES
January 24, 2008

o Southern Dunes and Spiders

http://hirise.lpl.arizona.edu/PSP_006538_1035

o Layered Sediments in Terby Crater

http://hirise.lpl.arizona.edu/PSP_006475_1525

o Splotches and Channels Near Sisyphi Montes

http://hirise.lpl.arizona.edu/PSP_005424_1075


o Polar Pit Gullies

http://hirise.lpl.arizona.edu/PSP_005410_1115


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, January 24, 2008

Giant Storm Eruption at Jupiter Unearths a Buried Past

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.

NEWS RELEASE: 2008-013 Jan. 24, 2008

Giant Storm Eruption at Jupiter Unearths a Buried Past

Scientists around the globe have observed an astonishing and rare change in Jupiter's
atmosphere -- a huge disturbance churning in the middle northern latitudes of the planet
as two giant storms erupted.

Jupiter's winds are the strongest at middle northern latitudes, reaching about 600
kilometers per hour (370 miles per hour). Similar phenomena occurred in 1975 and
1990, but this event has never been observed before with high-resolution modern
telescopes.

The storm eruption was captured in late March 2007 by NASA's Hubble Space
Telescope, the NASA Infrared Telescope Facility in Hawaii and telescopes in the
Canary Islands (Spain). A network of smaller telescopes around the world also
supported these observations.

An international team coordinated by Agustín Sánchez-Lavega from the Universidad
del País Vasco in Spain presents their findings about this event in the January 24 issue
of the journal Nature. The team monitored the new eruption of cloud activity and its
evolution with unprecedented resolution.

"Fortuitously, we captured the onset of the disturbance with Hubble, while monitoring
the planet to support the New Horizons flyby observations of Jupiter in its route to
Pluto. We saw the storm grow rapidly since its beginning, from about 400 kilometers
[250 miles] to more than 2,000 kilometers [1,245 miles] in size in less than one day,"
said Sánchez-Lavega.

The atmosphere of the gaseous giant planet Jupiter is always turbulent. Its circulation is
dominated by a pattern of cloud bands alternating with latitude, and by a persistent
system of jet streams, both of unknown origin. Changes in the cloud bands are
sometimes violent, starting from a localized eruption and followed by the development
of a planetary-scale disturbance. The nature of these disturbances and the power source
for these jets remains a controversial matter among planetary scientists and
meteorologists. The phenomena could be powered by the sun, as is Earth, by the strong
internal heat source emanating from Jupiter's interior, or by a combination of both.


According to the analysis, the bright plumes were storm systems triggered in Jupiter's
deep water clouds that vigorously moved upward in the atmosphere and injected a fresh
mixture of ammonia ice and water about 30 kilometers (20 miles) above the visible
clouds. The storms moved in the peak of a jet stream in Jupiter's atmosphere at 600
kilometers per hour (375 miles per hour). They disturbed the jet and formed in their
wake a turbulent planetary-scale disturbance containing red cloud particles.

"The infrared images distinguish the plumes from lower-altitude clouds and show that
the plumes are lofting ice particles higher than anyplace else on the planet," said Glenn
Orton of NASA's Jet Propulsion Laboratory, Pasadena, Calif. Orton is second author of
the paper.

In spite of the energy deposited and the stirring and turmoil generated by the storms, the
jet remained practically unchanged when the disturbance ceased, keeping steady against
these storms. Models of the disturbance indicate that the jet stream extends deep in the
buried atmosphere of Jupiter, more than 100 kilometers (62 miles) below the cloud tops
where most sunlight is absorbed.

"This confirms previous findings by the Galileo probe when it descended through
Jupiter's upper atmosphere in December 1995. Although both regions are
meteorologically different, all the evidence points to a deep extent for Jupiter's jets and
suggest that the internal heat power source plays a significant role in generating the jet,"
said Sánchez-Lavega.

A comparison of this disturbance with the two previous events in 1975 and 1990 shows
surprising similarities and coincidences, all of which remain unexplained. All three
eruptions occurred with a periodic interval of about 15 to 17 years. The plumes always
appear in the jet peak; the disturbance erupted with exactly two plumes. Finally, the
plumes moved with the same speed of the jet peak in all three events. Understanding
this outbreak could be the key to unlocking the mysteries buried in the deep Jovian
atmosphere.

Understanding these phenomena is important for Earth's meteorology, where storms are
present everywhere and jet streams dominate the atmospheric circulation. In this way,
Jupiter represents a natural laboratory where atmospheric scientists study the nature and
interplay of the intense jets and severe atmospheric phenomena.

For images, visit:

http://www.nasa.gov/topics/solarsystem/features/hubble20080123c.html and

http://hubblesite.org/newscenter/ .

JPL is managed for NASA by the California Institute of Technology. The Hubble
Space Telescope is a project of international cooperation between NASA and the
European Space Agency.

-end-

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Asteroid to Make Rare Close Flyby of Earth January 29

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

Grey Hautaluoma 202-358-0668
Headquarters, Washington
grey.hautaluoma-1@nasa.gov

NEWS RELEASE: 2008-012 Jan. 24, 2008

Asteroid to Make Rare Close Flyby of Earth January 29

Scientists are monitoring the orbit of asteroid 2007 TU24. The asteroid, believed to be between 150
meters (500 feet) and 610 meters (2,000 feet) in size, is expected to fly past Earth on Jan. 29, with its
closest distance being about 537,500 kilometers (334,000 miles) at 12:33 a.m. Pacific time (3:33 a.m.
Eastern time). It should be observable that night by amateur astronomers with modest-sized
telescopes.

Asteroid 2007 TU24 was discovered by the NASA-sponsored Catalina Sky Survey on Oct. 11, 2007.
Scientists at NASA's Near-Earth Object Program Office at the Jet Propulsion Laboratory in Pasadena,
Calif., have determined that there is no possibility of an impact with Earth in the foreseeable future.

"This will be the closest approach by a known asteroid of this size or larger until 2027," said Don
Yeomans, manager of the Near Earth Object Program Office at JPL. "As its closest approach is about
one-and-a-half times the distance of Earth to the moon, there is no reason for concern. On the
contrary, Mother Nature is providing us an excellent opportunity to perform scientific observations."

Asteroid 2007 TU24 will reach an approximate apparent magnitude 10.3 on Jan. 29-30 before
quickly becoming fainter as it moves farther from Earth. On that night, the asteroid will be
observable in dark and clear skies through amateur telescopes with apertures of at least 7.6
centimeters (3 inches). An object with a magnitude of 10.3 is about 50 times fainter than an object
just visible to the naked eye in a clear, dark sky.

NASA detects and tracks asteroids and comets passing close to Earth. The Near Earth Object
Observation Program, commonly called "Spaceguard," discovers, characterizes and computes
trajectories for these objects to determine if any could be potentially hazardous to our planet.

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


- end -


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Wednesday, January 23, 2008

Orbiting Camera Details Dramatic Wind Action on 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

Lori Stiles 520-626-4402
University of Arizona, Tucson
lstiles@u.arizona.edu

NEWS RELEASE: 2008-111 Jan. 23, 2008

Orbiting Camera Details Dramatic Wind Action on Mars

Mars has an ethereal, tenuous atmosphere with less than one-percent the surface pressure
of Earth, which challenges scientists to explain complex, wind-sculpted landforms seen
with unprecedented detail in images from NASA's Mars Reconnaissance Orbiter.

One of the main questions has been if winds on present-day Mars are strong enough to
form and change geological features, or if wind-constructed formations were made in the
past, perhaps when winds speeds and atmospheric pressures were higher.

The eye-opening new views of wind-driven Mars geology come from the University of
Arizona's High Resolution Imaging Science Experiment camera (HiRISE). As the orbiter
flies at about 3,400 meters per second (7,500 mph) between 250 and 315 kilometers (155
to 196 miles) above the Martian surface, this camera can see features as small as half a
meter (20 inches).

"We're seeing what look like smaller sand bedforms on the tops of larger dunes, and,
when we zoom in more, a third set of bedforms topping those," said HiRISE co-
investigator Nathan Bridges of NASA's Jet Propulsion Laboratory in Pasadena, Calif.
"On Earth, small bedforms can form and change on time scales as short as a day."

There are two kinds of "bedforms," or wind-deposited landforms. They can be sand
dunes, which are typically larger and have distinct shapes. Or they can be ripples, in
which sand is mixed with coarser particles. Ripples are typically smaller and more linear.

HiRISE also shows detail in sediments deposited by winds on the downwind side of
rocks. Such "windtails" show which way the most current winds have blown, Bridges
said. They have been seen before, but only by rovers and landers, never by an orbiter.
Researchers can now use HiRISE images to infer wind directions over the entire planet.

Scientists discovered miles-long, wind-scoured ridges called "yardangs" with the first
Mars orbiter, Mariner 9, in the early 1970s. New HiRISE images reveal surface texture
and fine-scale features that are giving scientists insight into how yardangs form.
"HiRISE is showing us just how interesting layers in yardangs are," Bridges said. "For
example, we see one layer that appears to have rocks in it. You can actually see rocks in
the layer, and if you look downslope, you can see rocks that we think have eroded out
from that rocky layer above."

New images show that some layers in the yardangs are made of softer materials that have
been modified by wind, he added. The soft material could be volcanic ash deposits, or the
dried-up remnants of what once were mixtures of ice and dust, or something else. "The
fact that we see layers that appear to be rocky and layers that are obviously soft says that
the process that formed yardangs is no simple process but a complicated sequence of
processes," Bridges said.

"HiRISE keeps showing interesting things about terrains that I expected to be
uninteresting," said Alfred McEwen of the University of Arizona Lunar and Planetary
Laboratory, HiRISE principal investigator. "I was surprised by the diversity of
morphology of the thick dust mantles. Instead of a uniform blanket of smooth dust, there
are often intricate patterns due to the action of the wind and perhaps light cementation
from atmospheric volatiles."

Paul Geissler of the U.S. Geological Survey, Flagstaff, Ariz., has discovered from
HiRISE images that dark streaks coming from Victoria Crater probably consist of streaks
of dark sand blown out from the crater onto the surface. Scientists had wondered if wind
might have blown away lighter-colored surface material, exposing a darker underlying
surface. Geissler is comparing HiRISE images to images taken by NASA's Mars
Exploration Rover Opportunity rover at Victoria Crater.

Bridges is lead author and McEwen is a co-author on the paper titled "Windy Mars: A
dynamic planet as seen by the HiRISE camera" in Geophysical Research Letters in
December.

Information about the Mars Reconnaissance Orbiter spacecraft is online at

http://www.nasa.gov/mro . The mission is managed by JPL, a division of the California
Institute of Technology, Pasadena, for the NASA Science Mission Directorate,
Washington, D.C. Lockheed Martin Space Systems, Denver, is the prime contractor and
built the spacecraft. Ball Aerospace & Technologies Corp., Boulder, Colo., built the
HiRISE camera operated by The University of Arizona, Tucson.

-end-

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Antarctic Ice Loss Speeds up, Nearly Matches Greenland Loss

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: 2008-010 Jan. 23, 2008

Antarctic Ice Loss Speeds up, Nearly Matches Greenland Loss

PASADENA, Calif. – Ice loss in Antarctica increased by 75 percent in the last 10 years due to a
speed-up in the flow of its glaciers and is now nearly as great as that observed in Greenland,
according to a new, comprehensive study by NASA and university scientists.

In a first-of-its-kind study, an international team led by Eric Rignot of NASA's Jet Propulsion
Laboratory, Pasadena, Calif., and the University of California, Irvine, estimated changes in
Antarctica's ice mass between 1996 and 2006 and mapped patterns of ice loss on a glacier-by-
glacier basis. They detected a sharp jump in Antarctica's ice loss, from enough ice to raise global
sea level by 0.3 millimeters (.01 inches) a year in 1996, to 0.5 millimeters (.02 inches) a year in
2006.

Rignot said the losses, which were primarily concentrated in West Antarctica's Pine Island Bay
sector and the northern tip of the Antarctic Peninsula, are caused by ongoing and past
acceleration of glaciers into the sea. This is mostly a result of warmer ocean waters, which bathe
the buttressing floating sections of glaciers, causing them to thin or collapse. "Changes in
Antarctic glacier flow are having a significant, if not dominant, impact on the mass balance of the
Antarctic ice sheet," he said.

To infer the ice sheet's mass, the team measured ice flowing out of Antarctica's drainage basins
over 85 percent of its coastline. They used 15 years of satellite radar data from the European
Earth Remote Sensing-1 and -2, Canada's Radarsat-1 and Japan's Advanced Land Observing
satellites to reveal the pattern of ice sheet motion toward the sea. These results were compared
with estimates of snowfall accumulation in Antarctica's interior derived from a regional
atmospheric climate model spanning the past quarter century.

The team found that the net loss of ice mass from Antarctica increased from 112 (plus or minus
91) gigatonnes a year in 1996 to 196 (plus or minus 92) gigatonnes a year in 2006. A gigatonne is
one billion metric tons, or more than 2.2 trillion pounds. These new results are about 20 percent
higher over a comparable time frame than those of a NASA study of Antarctic mass balance last
March that used data from the NASA/German Aerospace Center Gravity Recovery and Climate
Experiment. This is within the margin of error for both techniques, each of which has its
strengths and limitations.

Rignot says the increased contribution of Antarctica to global sea level rise indicated by the study
warrants closer monitoring.

"Our new results emphasize the vital importance of continuing to monitor Antarctica using a
variety of remote sensing techniques to determine how this trend will continue and, in particular,
of conducting more frequent and systematic surveys of changes in glacier flow using satellite
radar interferometry," Rignot said. "Large uncertainties remain in predicting Antarctica's future
contribution to sea level rise. Ice sheets are responding faster to climate warming than
anticipated."

Rignot said scientists are now observing these climate-driven changes over a significant fraction
of the West Antarctic Ice Sheet, and the extent of the glacier ice losses is expected to keep rising
in the years to come. "Even in East Antarctica, where we find ice mass to be in near balance, ice
loss is detected in its potentially unstable marine sectors, warranting closer study," he said.

Other organizations participating in the NASA-funded study, in addition to the University of
California, Irvine, are Centro de Estudios Cientificos, Valdivia, Chile; University of Bristol,
United Kingdom; Institute for Marine and Atmospheric Research, Utrecht University, Utrecht,
The Netherlands; University of Missouri, Columbia, Mo.; and the Royal Netherlands
Meteorological Institute, De Bilt, The Netherlands.

Results of the study are published in February's issue of Nature Geoscience.

Additional media contact for this story: Jennifer Fitzenberger, University of California, Irvine;
949-824-3969, jfitzen@uci.edu .

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

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

-end-


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Friday, January 18, 2008

Mars Odyssey THEMIS Images: January 14-18, 2008

MARS ODYSSEY THEMIS IMAGES
January 14-18, 2008

o End of Summer (Released 14 January 2008)

http://themis.asu.edu/zoom-20080114a

o Reynolds Crater (Released 15 January 2008)

http://themis.asu.edu/zoom-20080115a

o Russell Crater (Released 16 January 2008)

http://themis.asu.edu/zoom-20080116a

o Wirtz Crater (Released 17 January 2008)

http://themis.asu.edu/zoom-20080117a

o Hellas Dunes (Released 18 January 2008)

http://themis.asu.edu/zoom-20080118a

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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Thursday, January 17, 2008

NASA Tsunami Research Makes Waves in Science Community

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: 2008-007 Jan. 17, 2008

NASA Tsunami Research Makes Waves in Science Community

PASADENA, Calif. – A wave of new NASA research on tsunamis has yielded an innovative
method to improve existing tsunami warning systems, and a potentially groundbreaking new
theory on the source of the December 2004 Indian Ocean tsunami.

In one study, published last fall in Geophysical Research Letters, researcher Y. Tony Song of
NASA's Jet Propulsion Laboratory, Pasadena, Calif., demonstrated that real-time data from
NASA's network of global positioning system (GPS) stations can detect ground motions
preceding tsunamis and reliably estimate a tsunami's destructive potential within minutes, well
before it reaches coastal areas. The method could lead to development of more reliable global
tsunami warning systems, saving lives and reducing false alarms.

Conventional tsunami warning systems rely on estimates of an earthquake's magnitude to
determine whether a large tsunami will be generated. Earthquake magnitude is not always a
reliable indicator of tsunami potential, however. The 2004 Indian Ocean quake generated a huge
tsunami, while the 2005 Nias (Indonesia) quake did not, even though both had almost the same
magnitude from initial estimates. Between 2005 and 2007, five false tsunami alarms were issued
worldwide. Such alarms have negative societal and economic effects.

Song's method estimates the energy an undersea earthquake transfers to the ocean to generate a
tsunami by using data from coastal GPS stations near the epicenter. With these data, ocean floor
displacements caused by the earthquake can be inferred. Tsunamis typically originate at undersea
boundaries of tectonic plates near the edges of continents.

"Tsunamis can travel as fast as jet planes, so rapid assessment following quakes is vital to
mitigate their hazard," said Ichiro Fukumori, a JPL oceanographer not involved in the study.
"Song and his colleagues have demonstrated that GPS technology can help improve both the
speed and accuracy of such analyses."

Song's method works as follows: an earthquake's epicenter is located using seismometer data.
GPS displacement data from stations near the epicenter are then gathered to derive seafloor
motions. Based upon these data, local topography data and new theoretical developments, a new
"tsunami scale" measurement from one to 10 is generated, much like the Richter Scale used for
earthquakes. Song proposes using the scale to make a distinction between earthquakes capable of
generating destructive tsunamis from those unlikely to do so.

To demonstrate his methodology on real earthquake-tsunamis, Song examined three historical
tsunamis with well-documented ground motion measurements and tsunami observations: Alaska
in 1964; the Indian Ocean in 2004; and Nias Island, Indonesia in 2005. His method successfully
replicated all three. The data compared favorably with conventional seismic solutions that usually
take hours or days to calculate.

Song said many coastal GPS stations are already in operation, measuring ground motions near
earthquake faults in real time once every few seconds. "A coastal GPS network established and
combined with the existing International GPS Service global sites could provide a more reliable
global tsunami warning system than those available today," he said.

The theory behind the GPS study was published in the December 20 issue of Ocean Modelling.
Song and his team from JPL; the California Institute of Technology, Pasadena, Calif.; University
of California, Santa Barbara; and Ohio State University, Columbus, Ohio, theorized most of the
height and energy generated by the 2004 Indian Ocean tsunami resulted from horizontal, not
vertical, faulting motions. The study uses a 3-D earthquake-tsunami model based on seismograph
and GPS data to explain how the fault's horizontal motions might be the major cause of the
tsunami's genesis.

Scientists have long believed tsunamis form from vertical deformation of seafloor during
undersea earthquakes. However, seismograph and GPS data show such deformation from the
2004 Sumatra earthquake was too small to generate the powerful tsunami that ensued. Song's
team found horizontal forces were responsible for two-thirds of the tsunami's height, as observed
by three satellites (NASA's Jason, the U.S. Navy's Geosat Follow-on and the European Space
Agency's Environmental Satellite), and generated five times more energy than the earthquake's
vertical displacements. The horizontal forces also best explain the way the tsunami spread out
across the Indian Ocean. The same mechanism was also found to explain the data observed from
the 2005 Nias earthquake and tsunami.

Co-author C.K. Shum of Ohio State University said the study suggests horizontal faulting
motions play a much more important role in tsunami generation than previously believed. "If this
is found to be true for other tsunamis, we may have to revise some early views on how tsunamis
are formed and where mega tsunamis are likely to happen in the future," he said.

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

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