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

Authors

292

  1. MG
    Maarten G. Kleinhans

    Utrecht University, Netherlands

    9 publications · 698 citations

    9

    h-index

  2. MT
    Marco Tubino

    University of Trento, Italy

    7 publications · 678 citations

    7

    h-index

  3. RR
    Rodolfo Repetto

    University of Genoa, Italy

    5 publications · 540 citations

    5

    h-index

  4. DR
    Daniel R. Parsons

    University of Hull, United Kingdom

    4 publications · 252 citations

    4

    h-index

  5. MB
    Michele Bolla Pittaluga

    University of Genoa, Italy

    3 publications · 362 citations

    3

    h-index

1–5 of 292

Venues

  1. Earth Surface Processes and Landforms

    10 publications · 657 citations

    10

    h-index

  2. Water Resources Research

    9 publications · 929 citations

    9

    h-index

  3. Geophysical Research Letters

    5 publications · 408 citations

    5

    h-index

  4. Journal of Fluid Mechanics

    5 publications · 232 citations

    5

    h-index

  5. Journal of Hydraulic Engineering

    5 publications · 145 citations

    5

    h-index

1–5