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Estimation of Flash Flood Guidance Considering Uncertainties of Rainfall-Runoff Models

机译:考虑降雨径流模型不确定性的闪光洪水指导估算

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Nowdays, the flash flood is characterized as flood leading to damage caused by heavy rainfall for short duration, steep slope and impervious layer. Furthermore, in Korea, the flood damage risk by flash flood is increasing due to climate change. So, we could use the Flash Flood Guidance(FFG) which means the amount of effective rainfall needed for flash flood occurrence The FFG is calculated from rainfall-runoff relationship curve that is derived from rainfall-runoff model and threshold runoff. Therefore, the FFG can be changed largely by the rainfall-runoff models and their parameters. Here we used four different rainfall-runoff models. Also, the FFG can show different value by Threshold Source Area / Minimum Source Channel Length for calculating parameters of GcIUH, and by section of stream for calculating bank-full discharge. In this study, we analyzed the uncertainties on rainfall-runoff relationship derived from rainfall-runoff models and their parameters, threshold runoff, and existence and nonexistence of stream section. As a result, the derived confidence intervals for rainfall-runoff relationship curves show different shape and extent of interval. We performed the rainfall analysis as follows: First, we distributed probabilistic rainfall by 1hr, 3hr and 6hr using Huff method. But we can not draw rainfall-runoff relationship curve through one probabilistic rainfall. Therefore, we divided that into ten and derived rainfall-runoff relationship using each distributed probabilistic rainfall by rainfall duration. Then, we suggested the confidence interval on average of sampled rainfall through Monte Carlo simulation for uncertainty analysis of rainfall-runoff relationship curve. Next, we gave weighting factor to each four model and combined one. So, we can suggest one rainfall-runoff relationship curve from four rainfall-runoff models. And we compared FFG by change for value of CSA(Critical Source Area)/MSCL(Minimum
机译:现在,闪光洪水的特点是洪水导致短期降雨量造成的损坏,陡峭的坡度和渗透层。此外,在韩国,由于气候变化,Flash洪水的洪水损失风险正在增加。因此,我们可以使用Flash泛型指导(FFG),这意味着FFG的闪蒸洪水发生所需的有效降雨量来自降雨 - 径流模型和阈值径流的降雨 - 径流关系曲线。因此,FFG可以很大程度上被降雨 - 径流模型及其参数改变。在这里,我们使用了四种不同的降雨径流模型。而且,FFG可以通过阈值源区域/最小源通道长度来显示不同的值,用于计算GCIUH的参数,以及用于计算银行 - 完全放电的流部分。在这项研究中,我们分析了从降雨 - 径流模型的降雨 - 径流关系的不确定性,以及他们的参数,阈值径流以及流部分的存在和不存在。结果,降雨 - 径流关系曲线的衍生置信区间显示了不同的形状和间隔程度。我们如下进行降雨分析:首先,我们使用Huff方法将概率降雨分布1小时,3小时和6小时。但我们无法通过一个概率降雨来吸取降雨径流关系曲线。因此,我们将其分为十个并使用每个分布式概率降雨的降雨持续时间来实现的降雨径流关系。然后,我们建议通过Monte Carlo模拟平均采样降雨的置信区间,以进行降雨径流关系曲线的不确定性分析。接下来,我们将加权因子提供给每个四种模型并组合一个。因此,我们可以建议从四个降雨径流模型中的一个降雨 - 径流关系曲线。我们将FFG与CSA(关键源区)/ MSCL的值进行比较(最小值

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