Windblown Sediment Accumulation
Windblown Sediment Accumulation is a geological process denoting the deposition and progressive buildup of detrital particles transported by aeolian winds, distinguished within aeolian systems by its sensitivity to climatic, topographic, and vegetation controls over sediment entrainment, transport, and settling.
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Variable features on Mars, 2, Mariner 9 global results
Carl Sagan, J. Veverka, Paul L. Fox et al. · Journal of Geophysical Research Atmospheres · 1973 · 149 citations
Vatche P. Tchakerian · Geographical Journal · 1996 · 116 citations
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Chinese Academy of Sciences
Beijing, China
7 h-index
21 publications
854 citations

Cornell University
Ithaca, United States
5 h-index
58 publications
5.6K citations
Jet Propulsion Laboratory
Pasadena, United States
5 h-index
35 publications
3.4K citations
Arizona State University
Tempe, United States
5 h-index
43 publications
4.2K citations
University of Arizona
Tucson, United States
5 h-index
21 publications
1K citations

Ames Research Center
Mountain View, United States
5 h-index
28 publications
2.6K citations

Washington State University
Pullman, United States
3 h-index
5 publications
194 citations
Politecnico di Torino
Turin, Italy
3 h-index
7 publications
111 citations
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JGR · 4 publications · 470 citations
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