4.4 Article

Modelling the long-term geomorphic response to check dam failures in an alpine channel with CAESAR-Lisflood

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INTERNATIONAL JOURNAL OF SEDIMENT RESEARCH
卷 37, 期 5, 页码 687-700

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IRTCES
DOI: 10.1016/j.ijsrc.2022.04.005

关键词

Landscape evolution model; Check dam failure; Weather generator; Natural hazards

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This study uses a landscape evolution model to simulate check dam failures due to lack of maintenance. The results show that check dam failures can cause channel erosion and an increase in sediment yield. It may take a long time for the channel to reach equilibrium after multiple check dam failures. Therefore, the maintenance of check dams is crucial.
Globally, between 1950 and 2011 nearly 80,000 debris flow fatalities occurred in densely populated regions in mountainous terrain. Mitigation of these hazards includes the construction of check dams, which limit coarse sediment transport and in the European Alps number in the 100,000s. Check dam functionality depends on periodic, costly maintenance, but maintenance is not always possible and check dams often fail. As such, there is a need to quantify the long-term (10-100 years) geomorphic response of rivers to check dam failures. Here, for the first time, a landscape evolution model (CAESAR-Lisflood) driven by a weather generator is used to replicate check dam failures due to the lack of maintenance, check dam age, and flood occurrence. The model is applied to the Guerbe River, Switzerland, a pre-Alpine catchment containing 73 check dams that undergo simulated failure. Also presented is a novel method to calibrate CAESAR-Lisflood's hydrological component on this ungauged catchment. Using 100-year scenarios of check dam failure, the model indicates that check dam failures can produce 8 m of channel erosion and a 322% increase in sediment yield. The model suggests that after check dam failure, channel erosion is the remobilization of deposits accumulated behind check dams, and, after a single check dam failure channel equilibrium occurs in five years, but after many check dam failures channel equilibrium may not occur until 15 years. Overall, these findings support the continued maintenance of check dams. (c) 2022 International Research and Training Centre on Erosion and Sedimentation/the World Association for Sedimentation and Erosion Research. Published by Elsevier B.V. All rights reserved.

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