Forward Modeling of the Topography of Ice on Mars to Infer Basal Shear Stress Conditions

Details Forward Modeling of the Topography of Ice on Mars to Infer Basal Shear Stress Conditions Forward Modeling of the Topography of Ice on Mars to Infer Basal Shear Stress Conditions

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpi....38.2396b&link_type=abstract

38th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXVIII), held March 12-16, 2007 in League City, Texas

Physics

Scientific paper

A threshold-sliding model is used to reconstruct ice that has partially
covered impact craters located near or on the edges of the South Polar
Layered Deposits. Model results indicated a constant basal shear stress
of ~0.6 bars, almost one-third that foun

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