Surface Creep is a sediment transport mechanism within Aeolian sedimentology whereby coarse sand-sized particles are entrained by wind and move through intermittent saltation and rolling along the surface, distinguished from suspension and saltation by their limited trajectory height and persistent contact with the bed.
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2017–2026
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164
University of California, Berkeley
Berkeley, United States
11 h-index
31 publications
1.5K citations
United States Geological Survey
Reston, United States
10 h-index
19 publications
1.2K citations
Planetary Science Institute
Tucson, United States
8 h-index
27 publications
1.3K citations
Scripps Institution of Oceanography
La Jolla, United States
6 h-index
13 publications
806 citations
Centre National de la Recherche Scientifique
Paris, France
5 h-index
11 publications
531 citations
University of Colorado Boulder
Boulder, United States
5 h-index
10 publications
419 citations
Istanbul Technical University
Istanbul, Türkiye
5 h-index
7 publications
442 citations
University of California San Diego
San Diego, United States
5 h-index
9 publications
286 citations
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- Geophysical Research Letters
15 publications · 734 citations
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- Journal of Geophysical Research Solid Earth
9 publications · 588 citations
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- Bulletin of the Seismological Society of America
BSSA · 6 publications · 250 citations
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- Geophysical Journal International
GJI · 5 publications · 223 citations
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- Sedimentology
4 publications · 248 citations
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