Articles | Volume 23, issue 11
https://doi.org/10.5194/hess-23-4471-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-23-4471-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Future shifts in extreme flow regimes in Alpine regions
Manuela I. Brunner
CORRESPONDING AUTHOR
Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Birmensdorf ZH, Switzerland
Daniel Farinotti
Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Birmensdorf ZH, Switzerland
Laboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zürich, Zurich, Switzerland
Harry Zekollari
Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Birmensdorf ZH, Switzerland
Laboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zürich, Zurich, Switzerland
Laboratoire de Glaciologie, Université Libre de Bruxelles, Brussels, Belgium
Matthias Huss
Laboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zürich, Zurich, Switzerland
Department of Geosciences, University of Fribourg, Fribourg, Switzerland
Massimiliano Zappa
Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Birmensdorf ZH, Switzerland
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- Revealing the impacts of climate change on mountainous catchments through high-resolution modelling J. Moraga et al. 10.1016/j.jhydrol.2021.126806
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- Impacts of climate change on winter flood mechanisms: Spatial variability, trends, and bivariate frequency of rain-on-snow and soil frost T. Zaqout & H. Andradóttir 10.1016/j.jhydrol.2024.131439
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- Impacts of climate change on Swiss alluvial aquifers – A quantitative forecast focused on natural and artificial groundwater recharge by surface water infiltration J. Epting et al. 10.1016/j.hydroa.2022.100140
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Latest update: 20 Nov 2024
Short summary
River flow regimes are expected to change and so are extreme flow regimes. We propose two methods for estimating extreme flow regimes and show on a data set from Switzerland how these extreme regimes are expected to change. Our results show that changes in low- and high-flow regimes are distinct for rainfall- and melt-dominated regions. Our findings provide guidance in water resource planning and management.
River flow regimes are expected to change and so are extreme flow regimes. We propose two...