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Cross-Section of buried Carbon-Dioxide (CO2) Ice on Mars
Caption NASA:"This cross-section view of underground layers near Mars' South Pole is a radargram based on data from the Shallow Subsurface Radar (SHARAD) instrument on NASA's Mars Reconnaissance Orbiter. Researchers interpret the zone that is nearly free of radio-wave reflections (hence dark in the radargram) to be composed of frozen Carbon Dioxide, or "dry ice."

The newly found deposit of dry ice contains enough CO2 to dramatically increase the total amount of Atmosphere on Mars when it will vaporize, as climate models suggest it does at times when the Planet's Tilt increases. Mars' current Atmosphere is about 95% Carbon Dioxide, and this deposit contains up to about 80% as much Carbon Dioxide as the Atmosphere does.

This cross-section covers a transect about 330 Km (approx. 205 miles) long in a Region from about 86° to 87° South Latitude and 280° to 10° East Longitude. The vertical dimension of the graphic is time delay of the radar echoes. The depth of the tallest portion of the cross-section corresponds to about 20 microseconds difference in time delay, which can be converted to roughly 1,7 Km (a little more than 1 mile). 

(SHARAD was provided by the Italian Space Agency. Its operations are led by Sapienza University of Rome, and its data are analyzed by a joint U.S.-Italian science team. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for the NASA Science Mission Directorate, Washington. Lockheed Martin Space Systems, Denver, built the Spacecraft)
Parole chiave: Mars from orbit - South Pole

Cross-Section of buried Carbon-Dioxide (CO2) Ice on Mars

Caption NASA:"This cross-section view of underground layers near Mars' South Pole is a radargram based on data from the Shallow Subsurface Radar (SHARAD) instrument on NASA's Mars Reconnaissance Orbiter. Researchers interpret the zone that is nearly free of radio-wave reflections (hence dark in the radargram) to be composed of frozen Carbon Dioxide, or "dry ice."

The newly found deposit of dry ice contains enough CO2 to dramatically increase the total amount of Atmosphere on Mars when it will vaporize, as climate models suggest it does at times when the Planet's Tilt increases. Mars' current Atmosphere is about 95% Carbon Dioxide, and this deposit contains up to about 80% as much Carbon Dioxide as the Atmosphere does.

This cross-section covers a transect about 330 Km (approx. 205 miles) long in a Region from about 86° to 87° South Latitude and 280° to 10° East Longitude. The vertical dimension of the graphic is time delay of the radar echoes. The depth of the tallest portion of the cross-section corresponds to about 20 microseconds difference in time delay, which can be converted to roughly 1,7 Km (a little more than 1 mile).

(SHARAD was provided by the Italian Space Agency. Its operations are led by Sapienza University of Rome, and its data are analyzed by a joint U.S.-Italian science team. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for the NASA Science Mission Directorate, Washington. Lockheed Martin Space Systems, Denver, built the Spacecraft)

SouthPole-PIA11988.jpg South_Polar_Feature-PIA13727.jpg South_Pole-PIA13985.jpg Spirit-OrbitalView-20081009-MRO.jpg SubsurfaceIce-PIA12214.jpg
Informazioni sul file
Nome del file:South_Pole-PIA13985.jpg
Nome album:MareKromium / Mars Reconnaissance Orbiter (MRO)
Valutazione (1 voti):55555(Mostra dettagli)
Parole chiave:Mars / from / orbit / - / South / Pole
Copyright:NASA/JPL-Caltech/Sapienza University of Rome/Southwest Research Institute
Dimensione del file:113 KiB
Data di inserimento:Apr 23, 2011
Dimensioni:1775 x 380 pixels
Visualizzato:268 volte
URL:https://www.lunexit.it/gallery/displayimage.php?pid=28908
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