Details
Original language | English |
---|---|
Article number | 20160 |
Journal | Scientific reports |
Volume | 13 |
Publication status | Published - 17 Nov 2023 |
Abstract
Global change alters hydro-climatic conditions, affects land use, and contributes to more frequent droughts and floods. Large artificial reservoirs may effectively alleviate hydro-climatic extremes, but their storage capacities are threatened by sedimentation processes, which in turn are exacerbated by land use change. Envisioning strategies for sustainable reservoir management requires interdisciplinary model chains to emulate key processes driving sedimentation under global change scenarios. Therefore, we introduce a model chain for the long-term prediction of complex three-dimensional (3d) reservoir sedimentation considering concurrent catchment, hydro-climatic, and land-use conditions. Applied to a mountainous Mediterranean catchment, the model chain predicts increased sediment production and decreased discharge for high and medium emission pathways. Increased winter precipitation, accompanied by a transition from snowfall to rainfall, is projected to aggravate reduced summer precipitation, emphasizing a growing need for reservoirs. Additionally, higher winter precipitation proliferates sediment production and reservoir sedimentation. Land use change can outweigh the increased reservoir sedimentation originating from hydro-climatic change, which highlights the significance of localized actions to reduce sediment production. Finally, a 3d hydro-morphodynamic model provides insights into interactions between global change and reservoir sedimentation with spatially explicit information on future sedimentation patterns facilitating the implementation of management strategies.
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In: Scientific reports, Vol. 13, 20160, 17.11.2023.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - An interdisciplinary model chain quantifies the footprint of global change on reservoir sedimentation
AU - Mouris, Kilian
AU - Schwindt, Sebastian
AU - Pesci, María Herminia
AU - Wieprecht, Silke
AU - Haun, Stefan
N1 - Funding Information: This study was conducted within the DIRT-X project, which is part of AXIS, an ERA-NET initiated by JPI Climate and funded by FFG Austria, BMBF Germany, FORMAS Sweden, NWO NL, and RCN Norway with co-funding from the European Union (Grant No. 776608). The last author is indebted to the Baden-Württemberg Stiftung for financial support through the Elite Program for Postdocs. We also thank Nils Rüther, Kordula Schwarzwälder, Slaven Conevski, Behnam Balouchi, and Thomas Bosshard for providing input data, and Kristian Förster, Maria Fernanda Morales Oreamuno, Jadran Surac, André Maffert, and Anna Cerf for their help and productive discussions.
PY - 2023/11/17
Y1 - 2023/11/17
N2 - Global change alters hydro-climatic conditions, affects land use, and contributes to more frequent droughts and floods. Large artificial reservoirs may effectively alleviate hydro-climatic extremes, but their storage capacities are threatened by sedimentation processes, which in turn are exacerbated by land use change. Envisioning strategies for sustainable reservoir management requires interdisciplinary model chains to emulate key processes driving sedimentation under global change scenarios. Therefore, we introduce a model chain for the long-term prediction of complex three-dimensional (3d) reservoir sedimentation considering concurrent catchment, hydro-climatic, and land-use conditions. Applied to a mountainous Mediterranean catchment, the model chain predicts increased sediment production and decreased discharge for high and medium emission pathways. Increased winter precipitation, accompanied by a transition from snowfall to rainfall, is projected to aggravate reduced summer precipitation, emphasizing a growing need for reservoirs. Additionally, higher winter precipitation proliferates sediment production and reservoir sedimentation. Land use change can outweigh the increased reservoir sedimentation originating from hydro-climatic change, which highlights the significance of localized actions to reduce sediment production. Finally, a 3d hydro-morphodynamic model provides insights into interactions between global change and reservoir sedimentation with spatially explicit information on future sedimentation patterns facilitating the implementation of management strategies.
AB - Global change alters hydro-climatic conditions, affects land use, and contributes to more frequent droughts and floods. Large artificial reservoirs may effectively alleviate hydro-climatic extremes, but their storage capacities are threatened by sedimentation processes, which in turn are exacerbated by land use change. Envisioning strategies for sustainable reservoir management requires interdisciplinary model chains to emulate key processes driving sedimentation under global change scenarios. Therefore, we introduce a model chain for the long-term prediction of complex three-dimensional (3d) reservoir sedimentation considering concurrent catchment, hydro-climatic, and land-use conditions. Applied to a mountainous Mediterranean catchment, the model chain predicts increased sediment production and decreased discharge for high and medium emission pathways. Increased winter precipitation, accompanied by a transition from snowfall to rainfall, is projected to aggravate reduced summer precipitation, emphasizing a growing need for reservoirs. Additionally, higher winter precipitation proliferates sediment production and reservoir sedimentation. Land use change can outweigh the increased reservoir sedimentation originating from hydro-climatic change, which highlights the significance of localized actions to reduce sediment production. Finally, a 3d hydro-morphodynamic model provides insights into interactions between global change and reservoir sedimentation with spatially explicit information on future sedimentation patterns facilitating the implementation of management strategies.
UR - http://www.scopus.com/inward/record.url?scp=85176962692&partnerID=8YFLogxK
U2 - 10.1038/s41598-023-47501-1
DO - 10.1038/s41598-023-47501-1
M3 - Article
C2 - 37978239
AN - SCOPUS:85176962692
VL - 13
JO - Scientific reports
JF - Scientific reports
SN - 2045-2322
M1 - 20160
ER -