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.
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2017–2026
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Finite-amplitude alternate bars
Marco Colombini, G. Seminara, Marco Tubino · Journal of Fluid Mechanics · 1987 · 356 citations
Sedimentology and morphology of a low‐sinuosity river: Calamus River, Nebraska Sand Hills
John Bridge, Norman D. Smith, F. TRENT et al. · Sedimentology · 1986 · 186 citations
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University of Trento
Trento, Italy
13 h-index
29 publications
1.8K citations

Delft University of Technology
Delft, The Netherlands
9 h-index
15 publications
753 citations
United States Geological Survey
Reston, United States
6 h-index
9 publications
381 citations

Centre National de la Recherche Scientifique
Paris, France
6 h-index
16 publications
697 citations
Colorado State University
Fort Collins, United States
5 h-index
7 publications
424 citations
IHE Delft Institute for Water Education
Delft, The Netherlands
5 h-index
6 publications
378 citations
University of Illinois Urbana-Champaign
Urbana, United States
5 h-index
9 publications
478 citations
Deltares
Delft, The Netherlands
4 h-index
4 publications
316 citations
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22 publications · 1.8K citations
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15 publications · 836 citations
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5 publications · 115 citations
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5 publications · 1.4K citations
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