Orbiter observations point to "dry ice" snowfall on Mars
The carbon dioxide snowfalls occurred from clouds around the Red Planet's south pole in winter.
September 13, 2012
NASA’s Mars Reconnaissance Orbiter (MRO) data have given scientists the clearest evidence yet of carbon dioxide snowfalls on Mars. This reveals the only known example of carbon dioxide snow falling anywhere in our solar system.
Observations by NASA's Mars Reconnaissance Orbiter have detected carbon-dioxide snow clouds on Mars and evidence of carbon-dioxide snow falling to the surface. // Credit: NASA/JPL-Caltech
Frozen carbon dioxide, better known as “dry ice,” requires temperatures of about –193° Fahrenheit (–125° Celsius), which is much colder than needed for freezing water. Carbon dioxide snow reminds scientists that, although some parts of Mars may look quite Earth-like, the Red Planet is very different.
“These are the first definitive detections of carbon dioxide snow clouds,” said Paul Hayne of NASA’s Jet Propulsion Laboratory (JPL) in Pasadena, California. “We firmly establish the clouds are composed of carbon dioxide — flakes of martian air — and they are thick enough to result in snowfall accumulation at the surface.”
The snowfalls occurred from clouds around the Red Planet’s south pole in winter. The presence of carbon dioxide ice in Mars’ seasonal and residual southern polar caps has been known for decades. In 2008, NASA’s Phoenix Lander mission observed falling water-ice snow on northern Mars.
Hayne and six colleagues analyzed data gained by looking at clouds straight overhead and sideways with the Mars Climate Sounder, one of six instruments on MRO. This instrument records brightness in nine wavebands of visible and infrared light as a way to examine particles and gases in the martian atmosphere.
The data provide information about temperatures, particle sizes, and their concentrations. The new analysis is based on data from observations in the south polar region during southern Mars’ winter in 2006-2007, identifying a tall carbon dioxide cloud about 300 miles (500 kilometers) in diameter persisting over the pole and smaller, shorter-lived, lower-altitude carbon dioxide ice clouds at latitudes from 70° to 80° south.
“One line of evidence for snow is that the carbon dioxide ice particles in the clouds are large enough to fall to the ground during the lifespan of the clouds,” David Kass from JPL said. “Another comes from observations when the instrument is pointed toward the horizon, instead of down at the surface. The infrared spectra signature of the clouds viewed from this angle is clearly carbon dioxide ice particles, and they extend to the surface. By observing this way, the Mars Climate Sounder is able to distinguish the particles in the atmosphere from the dry ice on the surface.”
Mars’ south polar residual ice cap is the only place on Mars where frozen carbon dioxide persists on the surface year-round. Just how the carbon dioxide from Mars’ atmosphere gets deposited has been in question. It is unclear whether it occurs as snow or by freezing out at ground level as frost. These results show snowfall is especially vigorous on top of the residual cap.
“The finding of snowfall could mean that the type of deposition — snow or frost — is somehow linked to the year-to-year preservation of the residual cap,” Hayne said.