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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Main Authors: Kuzmin R. O, Zabalueva E. V
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Ice
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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spelling 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
institution Open Polar
collection Unknown
op_collection_id 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
author2 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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