Channel Bifurcation
Channel Bifurcation is a geomorphological process in which a single fluvial channel divides into two or more distributary channels, characterized by the partitioning of water and sediment flow at a junction within a deltaic system.
109
Publications
5.6K
Citations
292
Authors
164
Institutions
Publications per year
2017–2026
25
Variants
Distributary Bifurcation
109
1–5 of 109
292
9
h-index
7
h-index
5
h-index
4
h-index
3
h-index
1–5 of 292
164
Utrecht University
Utrecht, The Netherlands
10 h-index
24 publications
1.9K citations

University of Trento
Trento, Italy
8 h-index
15 publications
1.3K citations

University of Leeds
Leeds, United Kingdom
5 h-index
15 publications
948 citations
University of Illinois Urbana-Champaign
Urbana, United States
4 h-index
5 publications
173 citations
Université Claude Bernard Lyon 1
Villeurbanne, France
4 h-index
19 publications
650 citations
Laboratoire de Mécanique des Fluides et d'Acoustique
Écully, France
4 h-index
16 publications
548 citations

Delft University of Technology
Delft, The Netherlands
4 h-index
10 publications
288 citations

Centre National de la Recherche Scientifique
Paris, France
4 h-index
16 publications
548 citations
1–8 of 164
10 publications · 657 citations
10
h-index
9 publications · 929 citations
9
h-index
5 publications · 408 citations
5
h-index
5 publications · 232 citations
5
h-index
5 publications · 145 citations
5
h-index
1–5