Channel Bedforms
Channel Bedforms is a geomorphological construct that refers to the characteristic ridges, ripples, dunes, or other surface undulations formed by the interaction of flowing water and sediment within a fluvial channel, distinguishing it from static channel features by its dynamic origin and dependence on flow hydraulics and sediment transport processes.
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2017–2026
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University of Leeds
Leeds, United Kingdom
17 h-index
47 publications
4.2K citations
The University of Texas at Austin
Austin, United States
16 h-index
30 publications
2.2K citations
United States Geological Survey
Reston, United States
16 h-index
28 publications
2.5K citations

Centre National de la Recherche Scientifique
Paris, France
15 h-index
55 publications
2K citations

University of Aberdeen
Aberdeen, United Kingdom
14 h-index
38 publications
1.2K citations
Colorado State University
Fort Collins, United States
13 h-index
22 publications
1.4K citations

National Oceanography Centre
Southampton, United Kingdom
12 h-index
40 publications
3K citations
University College London
London, United Kingdom
11 h-index
22 publications
2.1K citations
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70 publications · 5.9K citations
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JSR · 60 publications · 5.4K citations
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