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- W2611115088 abstract "Cumulative rainfall, its duration and intensity have increased in the last few decades. One consequence of these increases is extreme events such as large-scale landslides, landslide lakes, sediment yields, and sediment movement. This study focuses on large-scale and long-term sediment transport and the corresponding topology changes. Two real cases are discussed and analyzed: (1) Shoufeng River in Hawlian County and (2) Taimaili River in Taitung County. Observational data from those two sites are used to analyze the sediment transport, topology change mechanism, and characteristics. Some of the characteristics that are analyzed are the plane pattern changes and vertical profile changes. The observational data indicate that large-scale sediment movement processes can last for decades resulting in changes in the river bed elevation and the scale of catchment. The erosion and deposition effects can be seen in different locations and times during this process. The mechanism of the changes is different from small-scale and medium-scale. Therefore, this study calls this process a large-scale process for river bed changes. The results of this study will provide a reference for disaster prevention planning." @default.
- W2611115088 created "2017-05-12" @default.
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- W2611115088 date "2017-05-06" @default.
- W2611115088 modified "2023-09-23" @default.
- W2611115088 title "Gravel Riverbed Processes Resulting from Large-Scale Landslides" @default.
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- W2611115088 doi "https://doi.org/10.1002/9781118971437.ch18" @default.
- W2611115088 hasPublicationYear "2017" @default.
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