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Characteristics of rainfall responsible for debris flows in Wenchuan Earthquake area

机译:汶川地震区泥石流的降雨特征

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The ability to forecast debris flows is important because of their frequent occurrence and potential for large-scale damage in the Wenchuan Earthquake-hit area. Accurate understanding of the characteristics of rainfall responsible for triggering debris flows is necessary for an effective early warning procedure. This study examined the general characteristics and spatiotemporal variation of rainfall events that responsible for debris flows. Analysis was performed on rainfall data extracted during 2008-2013. The results revealed that the rainfall thresholds for debris flows varied annually and showed tendency toward higher conditions required. The coefficient of variation of relevant rainfall events indicated that the characteristics of the rainstorms changed. In addition, the coefficient of deviation revealed the spatial variation of rainfall in subregions, which was attributed to differences of the local climatic conditions that control debris flow occurrence. The primary controlling rainfall indices for triggering debris flows were filtered, and the most suitable models for establishing rainfall thresholds were selected. Ultimately, the rainfall thresholds were obtained for each subregion within the study area.
机译:预测泥石流的能力很重要,因为在汶川地震灾区,泥石流频繁发生并可能造成大规模破坏。对于有效的预警程序,必须准确了解引起泥石流的降雨特征。这项研究检查了造成泥石流的降雨事件的一般特征和时空变化。对2008-2013年期间提取的降雨数据进行了分析。结果表明,泥石流的降雨阈值每年都在变化,并显示出需要更高条件的趋势。相关降雨事件的变化系数表明暴雨的特征发生了变化。此外,偏差系数揭示了次区域降雨的空间变化,这归因于控制泥石流发生的局部气候条件的差异。筛选了触发泥石流的主要控制降雨指数,并选择了最合适的模型来建立降雨阈值。最终,获得研究区域内每个子区域的降雨阈值。

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