Analysis of permafrost depths on Mars

Details Analysis of permafrost depths on Mars Analysis of permafrost depths on Mars

May 1984

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1984apg..book..115c&link_type=abstract

In NASA, Washington Advan. in Planetary Geol. p 115-132 (SEE N84-25567 15-91)

Physics

Environment Models, Heat Transmission, Low Temperature Environments, Mars Surface, Permafrost, Soils, Geotemperature, Ice Mapping, Moisture Content, Stratigraphy, Temperature Gradients, Thermodynamics

Scientific paper

Permafrost is defined as any soil or rock material, regardless of the amount of moisture content, that has remained below 273K for more than two years. Rossbacher and Judson (1981) modeled thicknesses of permafrost at latitudes of 10° increments. This paper reexamines the approach used by Rossbacher and Judson in analyzing the Martian thermal regime and extends the analysis.

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