Channel Pattern Change is a geomorphological process denoting the systematic alteration in the planform configuration of an alluvial channel network over time, distinguished by shifts in channel planform type, such as from meandering to braided or avulsive configurations, driven by changes in sediment transport, flow regime, or boundary conditions.
174
Publications
13.9K
Citations
404
Authors
218
Institutions
Publications per year
2017–2026
18
Parents
Publications
174
1–5 of 174
Authors
404
- PA
6
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- MG
4
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- RF
4
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- PJ
3
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3
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1–5 of 404
Institutions
218
Utrecht University
Utrecht, The Netherlands
7 h-index
13 publications
604 citations
Western University
London, Canada
6 h-index
7 publications
733 citations
Aberystwyth University
Aberystwyth, United Kingdom
5 h-index
7 publications
435 citations
University of Stirling
Stirling, United Kingdom
5 h-index
6 publications
338 citations
Chinese Academy of Sciences
Beijing, China
4 h-index
8 publications
204 citations
United States Geological Survey
Reston, United States
4 h-index
12 publications
546 citations
Polish Academy of Sciences
Warsaw, Poland
3 h-index
4 publications
690 citations
The University of Sydney
Sydney, Australia
3 h-index
4 publications
87 citations
1–8 of 218
Venues
- Earth Surface Processes and Landforms
27 publications · 3.2K citations
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- Geomorphology
19 publications · 1.1K citations
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- River Research and Applications
9 publications · 722 citations
9
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- Scientific investigations report
SIR · 5 publications · 73 citations
5
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- Geological Society London Special Publications
5 publications · 172 citations
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1–5