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Assessing the impact of uncertainty on flood risk estimates with reliability analysis using 1-D and 2-D hydraulic models

机译:使用一维和二维水力模型进行可靠性分析,评估不确定性对洪水风险估算的影响

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This paper addresses the use of reliability techniques such as Rosenblueth'sPoint-Estimate Method (PEM) as a practical alternative to more precise MonteCarlo approaches to get estimates of the mean and variance of uncertainflood parameters water depth and velocity. These parameters define the floodseverity, which is a concept used for decision-making in the context offlood risk assessment. The method proposed is particularly useful when thedegree of complexity of the hydraulic models makes Monte Carlo inapplicablein terms of computing time, but when a measure of the variability of theseparameters is still needed. The capacity of PEM, which is a special case ofnumerical quadrature based on orthogonal polynomials, to evaluate the firsttwo moments of performance functions such as the water depth and velocity isdemonstrated in the case of a single river reach using a 1-D HEC-RAS model.It is shown that in some cases, using a simple variable transformation,statistical distributions of both water depth and velocity approximate thelognormal. As this distribution is fully defined by its mean and variance,PEM can be used to define the full probability distribution function ofthese flood parameters and so allowing for probability estimations of floodseverity. Then, an application of the method to the same river reach using a2-D Shallow Water Equations (SWE) model is performed. Flood maps of mean andstandard deviation of water depth and velocity are obtained, and uncertaintyin the extension of flooded areas with different severity levels isassessed. It is recognized, though, that whenever application of Monte Carlomethod is practically feasible, it is a preferred approach.
机译:本文介绍了使用可靠性技术(例如Rosenblueth的点估计方法(PEM))作为更精确的MonteCarlo方法的实用替代方法,以获取不确定的洪水参数水深和速度的均值和方差的估计值。这些参数定义了洪水严重性,这是在洪水风险评估中用于决策的概念。当水力模型的复杂程度使Monte Carlo在计算时间方面不适用时,但是当仍然需要测量这些参数的可变性时,提出的方法特别有用。 PEM是基于正交多项式的数字正交的特例,用于评估性能函数的前两个时刻,例如使用1-D HEC-RAS模型在单个河段中演示的水深和流速,该能力结果表明,在某些情况下,使用简单的变量转换,水深和流速的统计分布都近似为对数正态分布。由于此分布由其均值和方差完全定义,因此可以使用PEM定义这些洪水参数的完整概率分布函数,从而可以对洪水严重性进行概率估计。然后,使用2-D浅水方程(SWE)模型将该方法应用于同一条河段。获得了水深和流速的均值和标准差的洪水图,并评估了不同严重程度的洪水区域扩展的不确定性。但是,已经认识到,只要应用蒙特卡洛法实际可行,这就是一种首选方法。

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