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GIS-based assessment of debris flow hazards in Kulekhani Watershed, Nepal

机译:基于GIS的Kulekhani流域葡萄酒流动危险评估,尼泊尔

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摘要

Debris flows are a hazardous natural calamity in mountainous regions of Nepal. Torrential rainfall within a very short period of the year is the main triggering factor for instability of slopes and initiation of landslides in these regions. Furthermore, the topography of the mountains and poor land use practices are additional factors that contribute to these instabilities. In this research, a GIS model has been developed to assess the debris flow hazard in mountainous regions of Nepal. Landslide-triggering threshold rainfall frequency is related to the frequency of landslides and the debris flow hazard in these mountains. Rainfall records from 1980 to 2013 are computed for one- to seven-day cumulative annual maximum rainfall. The expected rainfall for 1 in 10 to 1 in 1000 years of return periods is analyzed. The expected threshold rainfall is modeled in the GIS environment to identify the factor of safety of mountain slopes in a study watershed. A relation between the frequency of rainfall and debris flow hazard area is derived for return periods of 25, 50, 100, and 200 years. The debris flow hazard results from the analysis are compared with a known event in the watershed and found to agree. This method can be applied to anticipated rainfall-induced debris flow from the live rainfall record to warn the hazard-prone community in these mountains.
机译:碎片流动是尼泊尔山区的危险自然灾难。在一年中非常短的时间内暴雨是斜坡不稳定的主要触发因素,并在这些地区的山体滑坡开始。此外,山脉和贫瘠的土地利用实践的地形是促进这些不稳定性的额外因素。在这项研究中,已经开发了一种GIS模型来评估尼泊尔山区的碎片流动危险。滑坡触发阈值降雨频率与山体滑坡的频率和这些山脉的碎片流动危险有关。从1980年到2013年的降雨记录被计算为七天累计年度最大降雨量。分析了1000多年返回期内的10至1中的预期降雨。预期的阈值降雨是在GIS环境中建模的,以确定山坡在研究中的山坡安全因素。降雨和碎片流量危险区域之间的关系是推导出25,50,100和200年的返回期。分析中的碎片流动危险结果与流域中的已知事件进行比较,发现同意。这种方法可以应用于预期的降雨诱导的碎片流量,从现场降雨记录中发出警告这些山脉的危险群落。

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