Planetary and Space Science 5 r
and mid-latitude surface processes 10Ma ago. Conditions favoring an active layer are not predicted to be common in the next 10Ma. The much higher obliquity excursions 1973; Pewe, 1991), where the year-average surface tem-perature is below the water freezing point (e.g., Williams hundreds of meters t...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.547.7204 2023-05-15T17:56:08+02:00 Planetary and Space Science 5 r The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.7204 http://www.planetary.brown.edu/pdfs/3229.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.7204 http://www.planetary.brown.edu/pdfs/3229.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.planetary.brown.edu/pdfs/3229.pdf Mars Past climate Permafrost Cryoplanation text ftciteseerx 2016-01-08T11:22:04Z and mid-latitude surface processes 10Ma ago. Conditions favoring an active layer are not predicted to be common in the next 10Ma. The much higher obliquity excursions 1973; Pewe, 1991), where the year-average surface tem-perature is below the water freezing point (e.g., Williams hundreds of meters thick (e.g., Brown, 1970). The upper meter(s)-thick layer of the ground in permafrost regions can undergo a yearly freezing and thawing cycle; this is ARTICLE IN PRESSknown as the active layer (Fig. 1) (Miller and Black, 2003). In the spring, a thawing wave propagates downwards into the permafrost and in the fall and early winter, a freezing Text permafrost Unknown |
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English |
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Mars Past climate Permafrost Cryoplanation |
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Mars Past climate Permafrost Cryoplanation Planetary and Space Science 5 r |
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Mars Past climate Permafrost Cryoplanation |
description |
and mid-latitude surface processes 10Ma ago. Conditions favoring an active layer are not predicted to be common in the next 10Ma. The much higher obliquity excursions 1973; Pewe, 1991), where the year-average surface tem-perature is below the water freezing point (e.g., Williams hundreds of meters thick (e.g., Brown, 1970). The upper meter(s)-thick layer of the ground in permafrost regions can undergo a yearly freezing and thawing cycle; this is ARTICLE IN PRESSknown as the active layer (Fig. 1) (Miller and Black, 2003). In the spring, a thawing wave propagates downwards into the permafrost and in the fall and early winter, a freezing |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
title |
Planetary and Space Science 5 r |
title_short |
Planetary and Space Science 5 r |
title_full |
Planetary and Space Science 5 r |
title_fullStr |
Planetary and Space Science 5 r |
title_full_unstemmed |
Planetary and Space Science 5 r |
title_sort |
planetary and space science 5 r |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.7204 http://www.planetary.brown.edu/pdfs/3229.pdf |
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permafrost |
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permafrost |
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http://www.planetary.brown.edu/pdfs/3229.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.7204 http://www.planetary.brown.edu/pdfs/3229.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766164231083786240 |