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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's Point-Estimate Method (PEM) as a practical alternative to more precise Monte Carlo approaches to get estimates of the mean and variance of uncertain flood parameters water depth and velocity. These parameters define the flood severity, which is a concept used for decision-making in the context of flood risk assessment. The method proposed is particularly useful when the degree of complexity of the hydraulic models makes Monte Carlo inapplicable in terms of computing time, but when a measure of the variability of these parameters is still needed. The capacity of PEM, which is a special case of numerical quadrature based on orthogonal polynomials, to evaluate the first two moments of performance functions such as the water depth and velocity is demonstrated 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 the lognormal. As this distribution is fully defined by its mean and variance, PEM can be used to define the full probability distribution function of these flood parameters and so allowing for probability estimations of flood severity. Then, an application of the method to the same river reach using a 2-D Shallow Water Equations (SWE) model is performed. Flood maps of mean and standard deviation of water depth and velocity are obtained, and uncertainty in the extension of flooded areas with different severity levels is assessed. It is recognized, though, that whenever application of Monte Carlo method is practically feasible, it is a preferred approach.
机译:本文介绍了使用可靠性技术(例如罗森布鲁斯的点估计方法(PEM))作为更精确的蒙特卡洛方法的一种实用替代方法,以获取不确定洪水参数水深和流速的均值和方差的估计值。这些参数定义了洪水的严重性,这是在洪水风险评估的背景下用于决策的概念。当水力模型的复杂程度使蒙特卡洛在计算时间上不适用时,但仍需要测量这些参数的可变性时,提出的方法特别有用。在使用1-D HEC的单个河段情况下,证明了PEM(这是基于正交多项式的数字正交的特例)评估性能函数的前两个矩(例如水深和流速)的能力。 -RAS模型。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于对数正态。由于此分布完全由均值和方差定义,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,只要应用蒙特卡洛方法实际上可行,它就是一种首选方法。

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