Seasonal Variations of Snow
or, and surface frost reaches mid-latitudes in late winter (3). In early spring, as the surface receives more sunlight, surficial CO 2 sublimates back into the atmosphere, causing the frost line to retreat to high latitudes. The elevation of the north pole of Mars is 6 km lower than the south pole (...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.61.4083 2023-05-15T16:38:15+02:00 Seasonal Variations of Snow Depth On Mars David E. Smith Maria T. Zuber Gregory A. Neumann The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.61.4083 http://ltpwww.gsfc.nasa.gov/tharsis/smith_snow.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.61.4083 http://ltpwww.gsfc.nasa.gov/tharsis/smith_snow.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://ltpwww.gsfc.nasa.gov/tharsis/smith_snow.pdf text ftciteseerx 2016-01-08T14:25:54Z or, and surface frost reaches mid-latitudes in late winter (3). In early spring, as the surface receives more sunlight, surficial CO 2 sublimates back into the atmosphere, causing the frost line to retreat to high latitudes. The elevation of the north pole of Mars is 6 km lower than the south pole (4, 5). In the north during the summer, the temperature rises above the CO 2 condensation temperature, and dry ice frost deposited during the previous winter sublimes away, revealing a residual H 2 O ice cap (6, 7). In contrast, the southern polar region is colder and has a lower atmospheric pressure, and as a consequence its surface veneer of CO 2 does not completely sublime. A residual dry ice surface is observed even in summer (8), although observations of atmospheric water vapor during some years (9, 10) have been cited as evidence for at least some surficial H 2 O(11). Both polar regions contain layered terrains that are characterized by about 3 km of relief (5, 12) and are believed to Text Ice cap North Pole South pole Unknown North Pole South Pole |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
or, and surface frost reaches mid-latitudes in late winter (3). In early spring, as the surface receives more sunlight, surficial CO 2 sublimates back into the atmosphere, causing the frost line to retreat to high latitudes. The elevation of the north pole of Mars is 6 km lower than the south pole (4, 5). In the north during the summer, the temperature rises above the CO 2 condensation temperature, and dry ice frost deposited during the previous winter sublimes away, revealing a residual H 2 O ice cap (6, 7). In contrast, the southern polar region is colder and has a lower atmospheric pressure, and as a consequence its surface veneer of CO 2 does not completely sublime. A residual dry ice surface is observed even in summer (8), although observations of atmospheric water vapor during some years (9, 10) have been cited as evidence for at least some surficial H 2 O(11). Both polar regions contain layered terrains that are characterized by about 3 km of relief (5, 12) and are believed to |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Depth On Mars David E. Smith Maria T. Zuber Gregory A. Neumann |
spellingShingle |
Depth On Mars David E. Smith Maria T. Zuber Gregory A. Neumann Seasonal Variations of Snow |
author_facet |
Depth On Mars David E. Smith Maria T. Zuber Gregory A. Neumann |
author_sort |
Depth On Mars |
title |
Seasonal Variations of Snow |
title_short |
Seasonal Variations of Snow |
title_full |
Seasonal Variations of Snow |
title_fullStr |
Seasonal Variations of Snow |
title_full_unstemmed |
Seasonal Variations of Snow |
title_sort |
seasonal variations of snow |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.61.4083 http://ltpwww.gsfc.nasa.gov/tharsis/smith_snow.pdf |
geographic |
North Pole South Pole |
geographic_facet |
North Pole South Pole |
genre |
Ice cap North Pole South pole |
genre_facet |
Ice cap North Pole South pole |
op_source |
http://ltpwww.gsfc.nasa.gov/tharsis/smith_snow.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.61.4083 http://ltpwww.gsfc.nasa.gov/tharsis/smith_snow.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766028523126915072 |