Alternate Bars

Alternate Bars is a fluvial bedform morphology characterized by a series of elongated, sedimentary ridges that develop alternately along the downstream direction on opposite banks of an alluvial channel, distinguished from other bar types by their regular spacing, asymmetric cross-sectional profile, and role in driving channel curvature and sediment transport dynamics.

97

Publications

7.5K

Citations

207

Authors

114

Institutions

Publications per year

2017–2026

25

Authors

207

  1. MT
    Marco Tubino

    University of Trento, Italy

    8 publications · 904 citations

    8

    h-index

  2. WE
    W. E. Dietrich

    University of California, Berkeley, United States

    6 publications · 407 citations

    6

    h-index

  3. NC
    Nicolas Claude

    Laboratoire d'Hydraulique Saint-Venant, France

    5 publications · 224 citations

    5

    h-index

  4. JM
    Jonathan M. Nelson

    United States Geological Survey, United States

    5 publications · 216 citations

    5

    h-index

  5. PA
    Peter A. Nelson

    Colorado State University, United States

    5 publications · 251 citations

    5

    h-index

1–5 of 207

Venues

  1. Water Resources Research

    22 publications · 1.8K citations

    21

    h-index

  2. Earth Surface Processes and Landforms

    15 publications · 836 citations

    14

    h-index

  3. Sedimentology

    5 publications · 428 citations

    5

    h-index

  4. Journal of Geophysical Research Earth Surface

    5 publications · 115 citations

    5

    h-index

  5. Journal of Fluid Mechanics

    5 publications · 1.4K citations

    5

    h-index

1–5