Braided Rivers is a type of alluvial fluvial system characterized by a network of multiple interconnected, aggrading, and laterally migrating channels that are separated by transient, unvegetated or sparsely vegetated sediment bars, distinguishing it from meandering rivers by its high sediment load, steep gradient, and frequent channel instability.
488
Publications
38.2K
Citations
1K
Authors
491
Institutions
Publications per year
2017–2026
94
Variants
Braided Streams
Publications
488
1–5 of 488
Authors
1K
- PA
24
h-index
- WB
18
h-index
- PJ
17
h-index
- HP
12
h-index
- MT
12
h-index
1–5 of 1K
Institutions
491
Western University
London, Canada
22 h-index
48 publications
3.8K citations
Centre National de la Recherche Scientifique
Paris, France
22 h-index
81 publications
4.5K citations
University of Trento
Trento, Italy
21 h-index
46 publications
3.3K citations
University of Leeds
Leeds, United Kingdom
15 h-index
26 publications
3K citations
Queen Mary University of London
London, United Kingdom
14 h-index
20 publications
2.2K citations
Chinese Academy of Sciences
Beijing, China
14 h-index
32 publications
1K citations
University of Minnesota
Minneapolis, United States
13 h-index
19 publications
2.3K citations
National Institute of Water and Atmospheric Research
Auckland, New Zealand
12 h-index
24 publications
1.2K citations
1–8 of 491
Venues
- Water Resources Research
38 publications · 4.4K citations
33
h-index
- Earth Surface Processes and Landforms
48 publications · 4.1K citations
32
h-index
- Geomorphology
22 publications · 2.1K citations
21
h-index
- Journal of Sedimentary Research
JSR · 21 publications · 2.3K citations
18
h-index
- Sedimentology
14 publications · 1.8K citations
14
h-index
1–5