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.
Research article
| 
22 Jan 2018
Research article |
| 22 Jan 2018
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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- Contrasting Impacts of a Hotter and Drier Future on Streamflow and Catchment Scale Sediment Flux in the High Andes J. Slosson et al. 10.1029/2021JF006182
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- Sharp Increase of Extreme Turbidity Events Due To Deglaciation in the Subtropical Andes I. Vergara et al. 10.1029/2021JF006584
- Lake snow as a mercury methylation micro-environment in the oxic water column of a deep peri-alpine lake A. Gallorini & J. Loizeau 10.1016/j.chemosphere.2022.134306
- Substantial Increases in the Water and Sediment Fluxes in the Headwater Region of the Tibetan Plateau in Response to Global Warming D. Li et al. 10.1029/2020GL087745
- Hydroclimatic control on suspended sediment dynamics of a regulated Alpine catchment: a conceptual approach A. Costa et al. 10.5194/hess-22-3421-2018
- The effects of changing channel retention: Unravelling the mechanisms behind the spatial and temporal trends of suspended sediment in the Rhine basin J. Cox et al. 10.1002/esp.5929
- Making stratigraphy in the Anthropocene: climate change impacts and economic conditions controlling the supply of sediment to Lake Geneva S. Lane et al. 10.1038/s41598-019-44914-9
- Sediment yield over glacial cycles: A conceptual model G. Antoniazza & S. Lane 10.1177/0309133321997292
- Efficient multi-objective calibration and uncertainty analysis of distributed snow simulations in rugged alpine terrain J. Thornton et al. 10.1016/j.jhydrol.2021.126241
- The mineralization and sequestration of soil organic carbon in relation to gully erosion L. Cui et al. 10.1016/j.catena.2022.106218
- Climatic and hydrogeomorphic controls on sediment characteristics in the southern Sierra Nevada M. Safeeq et al. 10.1016/j.jhydrol.2022.128300
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- Shifted sediment-transport regimes by climate change and amplified hydrological variability in cryosphere-fed rivers T. Zhang et al. 10.1126/sciadv.adi5019
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- Environmental control of the present-day sediment export along the extratropical Andes I. Vergara et al. 10.1016/j.geomorph.2023.108911
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- Regional and Annual Variability in Subglacial Sediment Transport by Water for Two Glaciers in the Swiss Alps I. Delaney et al. 10.3389/feart.2018.00175
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- Subglacial Channels, Climate Warming, and Increasing Frequency of Alpine Glacier Snout Collapse P. Egli et al. 10.1029/2021GL096031
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- How do climate and land use change impact sediment yield in a Caspian Sea sub-basin? A. Daneshi et al. 10.1007/s13762-024-05501-2
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Latest update: 03 Mar 2025
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...
