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- W4301396502 abstract "<strong class=journal-contentHeaderColor>Abstract.</strong> The 2008 Wenchuan earthquake triggered local geomorphic changes rapidly and gradually and produced abundant materials through external processes. The abundant materials increased the risks of geomorphic hazards (flash floods, landslides, and debris flows) induced by extreme precipitation in the area. To reduce sediment transport present in geomorphic hazards, intervention measures such as dams, levees, and vegetation revetments have been constructed in specified sites. This study concentrated on the assessment of intervention effects incorporated with various facilities on post-earthquake fragile mountains in the short-medium term. Take the Xingping valley as an example, we used the CAESAR-Lisflood landscape evolution model to simulate three different scenarios including unprotected landscapes, present protected landscapes, and enhanced protected landscapes in 2011–2013. We compared the geomorphic changes and defined two indicators to assess the intervention effects. The results showed that the mitigation facilities were effective, especially engineering measures that cooperated with vegetation revetments in the upstream area, and the present mitigation measures were inadequate to stop materials loss and prevent hazards from the upstream area. Moreover, the effectiveness reduced gradually caused by the storage capacity of dams decreased. The simulation methods assessed the ability and effectiveness of cooperated control measures and could support optimum mitigation strategies." @default.
- W4301396502 created "2022-10-05" @default.
- W4301396502 creator A5071389166 @default.
- W4301396502 date "2022-10-04" @default.
- W4301396502 modified "2023-09-30" @default.
- W4301396502 title "Reply on RC1" @default.
- W4301396502 doi "https://doi.org/10.5194/nhess-2022-195-ac1" @default.
- W4301396502 hasPublicationYear "2022" @default.
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