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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ftciteseerx:oai:CiteSeerX.psu:10.1.1.549.7944 2023-05-15T16:36:44+02:00 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 Kuzmin R. O Zabalueva E. V The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.7944 http://web.ru/conf/khitariada/informbul-1/planet-5.engl.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.7944 http://web.ru/conf/khitariada/informbul-1/planet-5.engl.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://web.ru/conf/khitariada/informbul-1/planet-5.engl.pdf text ftciteseerx 2016-01-08T11:27:37Z 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 Text Ice permafrost Unknown |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
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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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Kuzmin R. O Zabalueva E. V |
spellingShingle |
Kuzmin R. O Zabalueva E. V 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 |
author_facet |
Kuzmin R. O Zabalueva E. V |
author_sort |
Kuzmin R. O |
title |
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 |
title_short |
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 |
title_full |
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 |
title_fullStr |
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 |
title_full_unstemmed |
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 |
title_sort |
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 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.7944 http://web.ru/conf/khitariada/informbul-1/planet-5.engl.pdf |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
http://web.ru/conf/khitariada/informbul-1/planet-5.engl.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.7944 http://web.ru/conf/khitariada/informbul-1/planet-5.engl.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766027061786312704 |