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Rainfall erosivity and sediment dynamics in the Himalaya catchment during the Melamchi flood in Nepal

Journal of Mountain Science 2023年第10期20卷 2993-3009页

作者： Binod BANIYA TANG Qiu-hong Bhupati NEUPANE XU Xi-meng HE Li Tirtha Raj ADHIKARI seyed rashid fallah shamsi Yam Prasad DHITAL Key Laboratory of Water Cycle and Related Land Surface Processes Institute of Geographic Sciences and Natural Resources ResearchChinese Academy of SciencesBeijing 1oo101China Department of Environmental Science Patan Multiple CampusInstitute of Science and TechnologyTribhuvan UniversityKathmandu44613Nepal State Key Laboratory of Tibetan Plateau Earth System Environment and ResourcesInstitute of Tibetan Plateau ResearchChine se Academy of SciencesBeijing 100101China Central Department of Hydrology and Meteorology Tribhuvan UniversityKathmandu 44613Nepal College of Applied Science Tribhuvan UniversityKathmandu 44613Nepal Department of Natural Resource and Environment College of AgricultureShiraz UniversityShiraz 71345Iran College of Water Resources and Architectural Engineering Shihezi UniversityShihezi 832000China

Rainfall erosivity is an indicator of rainfall potential to cause soil *** Melamchi extreme flood occurred on June-15 and recurred on July-31,2021 in *** these flooding events,a large volume of sediments were eroded,transported and deposited due to the high rainfall erosivity of the *** this study,the temporal and the spatial distribution of rainfall erosivity within the Melamchi River Basin was estimated and further linked to sediment discharge and concentration at various sites along the river *** daily rainfall data for the event year 2021 of the entire basin were *** was performed by post-flooding grain size *** result showed that rainfall and rainfall erosivity exhibit pronounced intensity within the Melamchi River basin,particularly at Sermathang and Tarkeghang,both located in the middle section of the *** average annual rainfall in the Melamchi region was 3140.39 mm with an average annual erosivity of 18302.06(MJ mm)/(ha h yr).The average daily erosivity of the basin was 358.67(MJ mm)/(ha h)during the first event and 1241(MJ mm)/(ha h)for the second *** the upper section of sampling,the sediment size ranged from 0.1 mm to>8 mm and was poorly ***,the lower region had smaller sediment ranging from 0.075 mm to>4.75 mm and also well *** smaller size(100 mm)sediments were passed relatively higher from the Kiwil(8.20%)and Ambathan(8.39%)river *** premonsoon and monsoon seasons,the highest sediment concentration was found to be 563.8 g/L and 344.3 g/L in Bhimtar and the lowest was 238.5 g/L and 132.1 g/L at the Ambathan,*** sediment concentration during the pre-monsoon was found to be higher than the sediment concentration during the monsoon season in the Melamchi *** more erosive regions in the basin were associated with the presence of highly

关键词： Rainfall erosivity Sediment Extreme flood Melamchi Nepal

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