Articles | Volume 14, issue 4
https://doi.org/10.5194/esurf-14-635-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esurf-14-635-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Lift or impact: modelling bedrock incision coupled with sediment dynamics
Philippe Davy
CORRESPONDING AUTHOR
Géosciences Rennes, Fractory, CNRS, Université de Rennes 1, Campus de Beaulieu, Rennes, France
Wolfgang Schwanghart
Institute of Environmental Science and Geography, University of Potsdam, Potsdam, Germany
Institute of Geographical Sciences, Freie Universität Berlin, Berlin, Germany
Jürgen Mey
Institute of Environmental Science and Geography, University of Potsdam, Potsdam, Germany
Caroline Darcel
Itasca consultants, Fractory, Campus de Beaulieu, Rennes, France
Angela Landgraf
National Cooperative for the Disposal of Radioactive Waste, Wettingen, Switzerland
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This study presents the results of an outdoor flume experiment to evaluate the effect of turbidity on the bleaching of fluvially transported sediment. Our main conclusions are that even small amounts of sediment lead to a substantial change in the intensity and frequency distribution of light within the suspension and that flow turbulence is an important prerequisite for bleaching grains during transport.
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During glacial times in Switzerland, glaciers of the Alps excavated valleys in low-lying regions that were later filled with sediment or water. How glaciers eroded these valleys is not well understood because erosion occurred near ice margins where ice moved slowly and was present for short times. Erosion is linked to the speed of ice and to water flowing under it. Here we present a model that estimates the location of water channels beneath the ice and links these locations to zones of erosion.
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Manuscript not accepted for further review
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The current socioeconomic development in the Himalayan region leads to a rapid expansion of the road network and an increase in the exposure to landslides. Our study along the NH-7 demonstrates the scale of this challenge as we detect more than one partially or fully road-blocking landslide per road kilometer. We identify the main controlling variables, i.e. slope angle, rainfall amount and lithology. As our approach uses a minimum of data, it can be extended to more complicated road networks.
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Short summary
The impact of sediment grains on the riverbed is a key driver of bedrock erosion yet is rarely included in studies of landscape evolution. We propose an equation to address this issue by considering the distinction between grain lift and grain impact. We solved and analysed these equations for simple cases, such as the downstream evolution of a riverbed, and implemented them in a numerical code that simulated the retreat of a knickpoint.
The impact of sediment grains on the riverbed is a key driver of bedrock erosion yet is rarely...