Melting of the Martian Permafrost by Hydrothermal Convection Associated with Magmatic Intrusion

Details Melting of the Martian Permafrost by Hydrothermal Convection Associated with Magmatic Intrusion Melting of the Martian Permafrost by Hydrothermal Convection Associated with Magmatic Intrusion

Jul 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003mars.conf.3095o&link_type=abstract

Sixth International Conference on Mars, July 20-25 2003, Pasadena, California, abstract no.3095

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Scientific paper

We quantitatively assessed the effect of thermal convection on enhancing
and focusing heat transfer in melting of the permafrost. The substantial
amount of meltwater could exist close to the surface, which should
affect the hydrothermal systems.

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