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Effects and consideration of storm movement in rainfall-runoff modelling at the basin scale

机译:流域尺度上暴雨运动对降雨-径流模拟的影响

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摘要

A number of studies have emphasized the effects of rainfall movement on runoff simulation; nevertheless, due to the lack of rain gauges inside sub-basins, a method using a hyetograph of the nearest gauges to a sub-basin is usually employed. This study investigated the effects of neglecting rainfall movement on overland simulation results in even a middle-sized basin. Simulations were carried out under two conditions: (1) stationary conditions where the nearest gauge hyetograph was used and rainfall movement was ignored, which is quite common in the case of a lack of data, and (2) moving conditions where a shifted hyetograph based on hyetograph timing recorded in the basin was used. The simulation results were compared with the measured discharge at the outlets. The results revealed that using the shifted hyetograph, which could consider the rainfall movement over sub-basins, decreased the mismatches between the simulated and observed hydrograph. In some of the cases, the shifted hyetograph reduced the relative difference more than 20 %. The study provided a useful method to cope with rainfall movement in runoff modelling of sparsely gauged large watersheds.
机译:许多研究强调了降雨运动对径流模拟的影响。然而,由于在子盆地内缺乏雨量计,通常采用一种使用与子盆地最接近的量表的刻线图的方法。这项研究调查了忽略降雨运动对中型盆地陆上模拟结果的影响。在以下两个条件下进行了模拟:(1)使用最接近的轨距距图的静止条件,而忽略了降雨运动,这在缺乏数据的情况下非常普遍;(2)在移动条件下,基于移动的距描仪使用在盆地记录的hyperograph定时。将模拟结果与出口处测得的流量进行比较。结果表明,使用移位的水位仪可以考虑降雨在子流域的运动,从而减少了模拟水位仪和观测水位仪之间的不匹配。在某些情况下,移位的离谱仪可将相对差异降低20%以上。该研究为稀疏大流域的径流模拟提供了一种有用的方法来应对降雨运动。

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