Reach-Scale Morphodynamics is a morphodynamic concept that characterizes the spatially integrated, scale-dependent processes of channel form adjustment and sediment transport dynamics over discrete, contiguous river segments, distinguished by its focus on reach-length scales where local hydraulics, boundary conditions, and sediment fluxes interact to produce geomorphologically meaningful changes in channel geometry.
129
Publications
9.5K
Citations
354
Authors
190
Institutions
Publications per year
2017–2026
35
Parents
Publications
129
Floods, channel change, and the hyporheic zone
Steven M. Wondzell, Frederick J. Swanson · Water Resources Research · 1999 · 1.4K citations · Full text
The morphology of riffle‐pool sequences
Keith Richards · Earth Surface Processes · 1976 · 247 citations
1–5 of 129
Authors
354
- JX
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- EW
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- SD
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1–5 of 354
Institutions
190
Wuhan University
Wuhan, China
9 h-index
42 publications
2.1K citations
University of British Columbia
Vancouver, Canada
9 h-index
23 publications
1.8K citations
Colorado State University
Fort Collins, United States
8 h-index
16 publications
1.1K citations
University of Glasgow
Glasgow, United Kingdom
8 h-index
12 publications
865 citations
Utah State University
Logan, United States
5 h-index
14 publications
423 citations
University of Illinois Urbana-Champaign
Urbana, United States
5 h-index
9 publications
481 citations
University of Padua
Padua, Italy
4 h-index
11 publications
256 citations
University of Trento
Trento, Italy
4 h-index
12 publications
539 citations
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Venues
- Earth Surface Processes and Landforms
27 publications · 1.4K citations
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- Geomorphology
23 publications · 1.4K citations
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- Water Resources Research
13 publications · 2.2K citations
13
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- River Research and Applications
6 publications · 262 citations
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- Journal of Geophysical Research Atmospheres
JGR · 5 publications · 1K citations
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