DETERMINING RATES OF RESURFACING BY WIND ON MARS HINGES UPON OUR UNDERSTANDING OF HOW SAND MOVES UNDER MARTIAN SURFACE CONDITIONS. THE CURRENT UNDERSTANDING OF AEOLIAN SEDIMENT TRANSPORT ON MARS LARGELY RELIES ON AEOLIAN SEDIMENT TRANSPORT MODELS FOR ESTI
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DETERMINING RATES OF RESURFACING BY WIND ON MARS HINGES UPON OUR UNDERSTANDING OF HOW SAND MOVES UNDER MARTIAN SURFACE CONDITIONS. THE CURRENT UNDERSTANDING OF AEOLIAN SEDIMENT TRANSPORT ON MARS LARGELY RELIES ON AEOLIAN SEDIMENT TRANSPORT MODELS FOR ESTI