Channel Incision

Channel incision is a geomorphological process characterized by the downward erosion of a riverbed into underlying strata, distinguished from lateral erosion by its vertical entrenchment of the channel profile in response to changes in flow, sediment load, or base level.

269

Publications

22.7K

Citations

781

Authors

396

Institutions

Publications per year

2017–2026

65

Variants

Stream Incision

Authors

781

  1. FD
    F. Douglas Shields

    National Sedimentation Laboratory, United States

    8 publications · 373 citations

    8

    h-index

  2. WE
    W. E. Dietrich

    University of California, Berkeley, United States

    7 publications · 2.1K citations

    7

    h-index

  3. KX
    K. X. Whipple

    Arizona State University, United States

    7 publications · 1.5K citations

    7

    h-index

  4. BW
    Bartłomiej Wyżga‬‬

    Polish Academy of Sciences, Poland

    6 publications · 402 citations

    6

    h-index

  5. SS
    Scott S. Knight

    National Sedimentation Laboratory, United States

    6 publications · 346 citations

    6

    h-index

1–5 of 781

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 22 publications · 4.1K citations

    21

    h-index

  2. Earth Surface Processes and Landforms

    24 publications · 2.1K citations

    20

    h-index

  3. Journal of Geophysical Research Earth Surface

    20 publications · 1.1K citations

    16

    h-index

  4. Geomorphology

    12 publications · 1.2K citations

    12

    h-index

  5. Water Resources Research

    11 publications · 2.5K citations

    11

    h-index

1–5