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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山洪指导量估算

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Nowdays, the flash flood is characterized as flood leading to damagecaused by heavy rainfall for short duration, steep slope and impervious layer.Furthermore, in Korea, the flood damage risk by flash flood is increasing due toclimate change. So, we could use the Flash Flood Guidance(FFG) which means theamount of effective rainfall needed for flash flood occurrenceThe FFG is calculated from rainfall-runoff relationship curve that is derived fromrainfall-runoff model and threshold runoff. Therefore, the FFG can be changedlargely by the rainfall-runoff models and their parameters. Here we used fourdifferent rainfall-runoff models. Also, the FFG can show different value byThreshold Source Area / Minimum Source Channel Length for calculatingparameters of GcIUH, and by section of stream for calculating bank-full discharge.In this study, we analyzed the uncertainties on rainfall-runoff relationship derivedfrom rainfall-runoff models and their parameters, threshold runoff, and existenceand nonexistence of stream section.As a result, the derived confidence intervals for rainfall-runoff relationship curvesshow different shape and extent of interval. We performed the rainfall analysis asfollows: First, we distributed probabilistic rainfall by 1hr, 3hr and 6hr using Huffmethod. But we can not draw rainfall-runoff relationship curve through oneprobabilistic rainfall. Therefore, we divided that into ten and derived rainfall-runoffrelationship using each distributed probabilistic rainfall by rainfall duration. Then,we suggested the confidence interval on average of sampled rainfall through MonteCarlo simulation for uncertainty analysis of rainfall-runoff relationship curve. Next,we gave weighting factor to each four model and combined one. So, we can suggestone rainfall-runoff relationship curve from four rainfall-runoff models. And wecompared FFG by change for value of CSA(Critical Source Area)/MSCL(Minimum
机译:如今,山洪的特征是洪灾导致破坏 由短时降雨,陡坡和不透水层引起。 此外,在韩国,由于 气候变化。因此,我们可以使用Flash Flood Guidance(FFG),这意味着 山洪暴发所需的有效降雨量 FFG是根据以下公式得出的降雨-径流关系曲线计算的 降雨径流模型和阈值径流。因此,可以更改FFG 主要由降雨径流模型及其参数决定。这里我们用了四个 不同的降雨径流模型。此外,FFG可以通过 阈值源面积/最小源通道长度,用于计算 GcIUH的参数,并按流段计算岸满流量。 在这项研究中,我们分析了得出的降雨-径流关系的不确定性 降雨径流模型及其参数,阈值径流和存在 流部分不存在。 结果,得出降雨-径流关系曲线的置信区间 显示不同的形状和间隔程度。我们进行了降雨分析 如下:首先,我们使用霍夫效应分别分配了1小时,3小时和6小时的概率降雨 方法。但是我们不能一一画出降雨-径流关系曲线 概率降雨。因此,我们将其分为十个,并得出降雨径流 使用每个降雨持续时间的分布概率降雨之间的关系。然后, 我们建议通过蒙特的平均降水量的置信区间 Carlo模拟用于降雨-径流关系曲线的不确定性分析。下一个, 我们将加权因子分配给每个四个模型,然后将其合并。所以,我们可以建议 来自四个降雨-径流模型的一条降雨-径流关系曲线。和我们 通过更改CSA(关键源区域)/ MSCL(最小)值来比较FFG

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