The solar-powered Phoenix lander operated for two months longer than its planned three-month mission in the Martian arctic in 2008. It was not designed to withstand winter conditions. However, in case the return of abundant springtime sunlight to the site does revive Phoenix, Odyssey is conducting three periods of listening for a transmission that Phoenix is programmed to send if it is able. The second listening period, with 60 overflights of the Phoenix site from Feb. 22 to Feb. 26, produced the same result as the first listening period in January: no signal heard.
The Space Foundation has awarded its 2009 John L. "Jack" Swigert, Jr., Award for Space Exploration to NASA's Phoenix Mars Lander team "in recognition of the technical developments that led to one of the most startling and meaningful discoveries of the new millennium," the Space Foundation announced today.
The award will be presented at the foundation's 25th National Space Symposium to be held in Colorado Springs, Colo., on March 30.
It honors the memory of Jack Swigert, the Apollo 13 command module pilot on the 1970 manned lunar-landing mission crew that successfully returned to Earth despite great hardship caused by an electrical explosion that crippled the spacecraft.
"It is a tremendous honor to win this award that honors a great American space hero who had a bold vision, but was given slim odds for success," said Peter H. Smith of The University of Arizona's Lunar and Planetary Laboratory, principal investigator for the Phoenix Mars Mission.
Last month, the Phoenix Mars Lander sent its final signal after working for 151 Martian days photographing, digging and testing samples in the arctic there. During those days, its findings reshaped what we know about Mars, the prospects of future space exploration and our approach to undertaking that mission. All reports provide reason for optimism about the scientific advances of the United States and the world, as well as excitement about the future for those of us involved in this landmark NASA mission.
For the first time, we touched water ice on Mars. We excavated it, examined its depth and studied how it changes over the surface. We found that Martian soil is alkaline (like that of Earth's dry climates) and contains carbonates and clays. In addition, nutrients and chemical energy sources that fuel microbes on the Earth are available in Martian soil. We now know that liquid water has been a part of this soil, and further review of our data will enable us to determine whether this can be considered a habitable zone on Mars where microbial communities could live in warmer periods and survive the colder times in a dormant state.