Articles | Volume 22, issue 1
https://doi.org/10.5194/hess-22-509-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/hess-22-509-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Temperature signal in suspended sediment export from an Alpine catchment
Institute of Environmental Engineering, ETH Zurich, 8093 Zurich,
Switzerland
Peter Molnar
Institute of Environmental Engineering, ETH Zurich, 8093 Zurich,
Switzerland
Laura Stutenbecker
Institute of Applied Geosciences, Technische Universität Darmstadt, Darmstadt, Germany
Maarten Bakker
Institute of Earth Surface Dynamics, University of Lausanne, 1015
Lausanne, Switzerland
Tiago A. Silva
Department F.-A. Forel for Environmental and Aquatic Sciences,
University of Geneva, 1211 Geneva, Switzerland
Fritz Schlunegger
Institute of Geological Sciences, University of Bern, 3012 Bern,
Switzerland
Stuart N. Lane
Institute of Earth Surface Dynamics, University of Lausanne, 1015
Lausanne, Switzerland
Jean-Luc Loizeau
Department F.-A. Forel for Environmental and Aquatic Sciences,
University of Geneva, 1211 Geneva, Switzerland
Stéphanie Girardclos
Department of Earth Sciences and Institute for Environmental Sciences,
University of Geneva, 1205 Geneva, Switzerland
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Latest update: 20 Nov 2024
Short summary
We explore the signal of a warmer climate in the suspended-sediment dynamics of a regulated and human-impacted Alpine catchment. We demonstrate that temperature-driven enhanced melting of glaciers, which occurred in the mid-1980s, played a dominant role in suspended sediment concentration rise, through increased runoff from sediment-rich proglacial areas, increased contribution of sediment-rich meltwater, and increased sediment supply in proglacial areas due to glacier recession.
We explore the signal of a warmer climate in the suspended-sediment dynamics of a regulated and...