PASADENA, Calif. (NASA PR) — What’s the sound of a touchdown on Mars?
If you’re at NASA’s Jet Propulsion Laboratory, it sounds like winning the Super Bowl: cheers, laughter and lots of hollering.
But in the minutes before that, NASA’s InSight team will be monitoring the Mars lander’s radio signals using a variety of spacecraft — and even radio telescopes here on Earth — to suss out what’s happening 91 million miles (146 million km) away.
NASA’s Mars Odyssey, which launched in 2001, will break the record Wednesday for longest-serving spacecraft at the Red Planet. The probe begins its 3,340th day in Martian orbit at 8:55 p.m. EST on Wednesday to break the record set by NASA’s Mars Global Surveyor, which orbited Mars from 1997 to 2006.
Odyssey’s longevity enables continued science, including the monitoring of seasonal changes on Mars from year to year and the most detailed maps ever made of most of the planet. In 2002, the spacecraft detected hydrogen just below the surface throughout Mars’ high-latitude regions. The deduction that the hydrogen is in frozen water prompted NASA’s Phoenix Mars Lander mission, which confirmed the theory in 2008. Odyssey also carried the first experiment sent to Mars specifically to prepare for human missions, and found radiation levels around the planet from solar flares and cosmic rays are two to three times higher than around Earth.
WASHINGTON – NASA’s Mars Odyssey orbiter has found evidence of salt deposits. These deposits point to places where water once was abundant and where evidence might exist of possible Martian life from the Red Planet’s past.
A team led by Mikki Osterloo of the University of Hawaii, Honolulu, found approximately 200 places on southern Mars that show spectral characteristics consistent with chloride minerals. Chloride is part of many types of salt, such as sodium chloride or table salt. The sites range from about half of a square mile to 25 times that size.
“They could come from groundwater reaching the surface in low spots,” Osterloo said. “The water would evaporate and leave mineral deposits, which build up over years. The sites are disconnected, so they are unlikely to be the remnants of a global ocean.”