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Tuesday, May 13, 2008

NASA Phoenix Mission Ready for Mars Landing

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
NASA Headquarters, Washington
dwayne.c.brown@nasa.gov

Sara Hammond 520-626-1974
University of Arizona, Tucson
shammond@lpl.arizona.edu

NEWS RELEASE: 2008-074 May 13, 2008

NASA Phoenix Mission Ready for Mars Landing

WASHINGTON -- NASA's Phoenix Mars Lander is preparing to end its long journey and begin a
three-month mission to taste and sniff fistfuls of Martian soil and buried ice. The lander is scheduled
to touch down on the Red Planet May 25.

Phoenix will enter the top of the Martian atmosphere at almost 21,000 kilometers per hour (almost
13,000 mph). In seven minutes, the spacecraft must complete a challenging sequence of events to
slow to about 8 kilometers per hour (5 mph) before its three legs reach the ground. Confirmation of
the landing could come as early as 4:53 p.m. PDT (7:53 p.m. EDT).

"This is not a trip to grandma's house. Putting a spacecraft safely on Mars is hard and risky," said Ed
Weiler, associate administrator for NASA's Science Mission Directorate at NASA Headquarters in
Washington. "Internationally, fewer than half the attempts have succeeded."

Rocks large enough to spoil the landing or prevent opening of the solar panels present the biggest
known risk. However, images from the High Resolution Imaging Science Experiment (HiRISE)
camera on NASA's Mars Reconnaissance Orbiter, detailed enough to show individual rocks smaller
than the lander, have helped lessen that risk.

"We have blanketed nearly the entire landing area with HiRISE images," said Ray Arvidson of
Washington University in St. Louis, chairman of the Phoenix landing-site working group.
"This is one of the least rocky areas on all of Mars and we are confident that rocks will not
detrimentally impact the ability of Phoenix to land safely."

Phoenix uses hardware from a spacecraft built for a 2001 launch that was canceled in response to the
loss of a similar Mars spacecraft during a 1999 landing attempt. Researchers who proposed the
Phoenix mission in 2002 saw the unused spacecraft as a resource for pursuing a new science
opportunity.

Earlier in 2002, NASA's Mars Odyssey orbiter discovered that plentiful water ice lies just beneath
the surface throughout much of high-latitude Mars. NASA chose the Phoenix proposal over 24 other
proposals to become the first endeavor in the Mars Scout program of competitively selected
missions. "Phoenix will land farther north on Mars than any previous mission," said Phoenix Project
Manager Barry Goldstein of NASA's Jet Propulsion Laboratory, Pasadena, Calif.

"The Phoenix mission not only studies the northern permafrost region, but takes the next step in
Mars exploration by determining whether this region, which may encompass as much as 25 percent
of the Martian surface, is habitable," said Peter Smith, Phoenix principal investigator at the
University of Arizona, Tucson.

The solar-powered robotic lander will manipulate a 2.35 meter arm (7.7 foot) to scoop up samples of
underground ice and soil lying above the ice. Onboard laboratory instruments will analyze the
samples. Cameras and a Canadian-supplied weather station will supply other information about the
site's environment.

One research goal is to assess whether conditions at the site ever have been favorable for microbial
life. The composition and texture of soil above the ice could give clues to whether the ice ever melts
in response to long-term climate cycles. Another important question is whether the scooped-up
samples contain carbon-based chemicals that are potential building blocks and food for life.

The Phoenix mission is led by Smith, with project management at JPL. The development partnership
is with Lockheed Martin, Denver. International contributions are from the Canadian Space Agency;
the University of Neuchatel, Switzerland; the universities of Copenhagen and Aarhus, Denmark; the
Max Planck Institute, Germany; and the Finnish Meteorological Institute.

For more about the Phoenix mission on the Web, visit:

http://www.nasa.gov/phoenix

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