1 NUMERICAL MODELLING OF THE ICE REDISTRIBUTION PROCESS WITHIN THE SURFACE LAYER OF THE REGOLITH ON THE MARS (EQUATOR) BY QUASI-PERIODIC OSCILLATIONS OF THE QBLIQUITY

The permafrost on Mars is globally widespread and its thickness may to approach 1-2 km in the equatorial zone and up to 6 km in the polar area [1, 2]. The permafrost may to be as one of the largest reservoir of the water ice, salt solution and gashydrates on the planet [2, 3]. Under modern climatic...

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Bibliographic Details
Main Authors: Kuzmin R. O, Zabalueva E. V
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Ice
permafrost
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.7944
http://web.ru/conf/khitariada/informbul-1/planet-5.engl.pdf
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Summary:The permafrost on Mars is globally widespread and its thickness may to approach 1-2 km in the equatorial zone and up to 6 km in the polar area [1, 2]. The permafrost may to be as one of the largest reservoir of the water ice, salt solution and gashydrates on the planet [2, 3]. Under modern climatic condition of Mars the ice in shallow regolith may to be stable (with respect to sublimation) in the both

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