Channel Bedforms

Channel Bedforms is a geomorphological construct that refers to the characteristic ridges, ripples, dunes, or other surface undulations formed by the interaction of flowing water and sediment within a fluvial channel, distinguishing it from static channel features by its dynamic origin and dependence on flow hydraulics and sediment transport processes.

647

Publications

45.3K

Citations

1.4K

Authors

616

Institutions

Publications per year

2017–2026

100

Authors

1.4K

  1. EW
    Ellen Wohl

    Colorado State University, United States

    9 publications · 703 citations

    9

    h-index

  2. JB
    John Bridge

    Binghamton University, United States

    9 publications · 1.6K citations

    9

    h-index

  3. JG
    Jeremy G. Venditti

    Simon Fraser University, Canada

    6 publications · 327 citations

    6

    h-index

  4. JB
    Jim Best

    University of Illinois Urbana-Champaign, United States

    6 publications · 960 citations

    6

    h-index

  5. DB
    Daryl B. Simons

    Colorado State University, United States

    6 publications · 1.1K citations

    6

    h-index

1–5 of 1.4K

Venues

  1. Sedimentology

    70 publications · 5.9K citations

    41

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  2. Journal of Sedimentary Research

    JSR · 60 publications · 5.4K citations

    37

    h-index

  3. Earth Surface Processes and Landforms

    34 publications · 2.7K citations

    25

    h-index

  4. Water Resources Research

    31 publications · 2.5K citations

    22

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  5. AAPG Bulletin

    22 publications · 2.1K citations

    21

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1–5