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On Latin Hypercube sampling for efficient uncertainty estimation of satellite rainfall observations in flood prediction

机译:基于拉丁超立方采样的洪水预报中卫星降雨观测的有效不确定性估计

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With the advent of the Global Precipitation Measurement (GPM) in 2009, satellite rainfall measurements are expected to become globally available at space-time scales relevant for flood prediction of un-gauged watersheds. For uncertainty assessment of such retrievals in flood prediction, error models need to be developed that can characterize the satellite's retrieval error structure. A full-scale assessment would require a large number of Monte Carlo (MC) runs of the satellite error model realizations, each passed through a hydrologic model, in order to derive the probability distribution in runoff. However, for slow running hydrologic models this can be computationally expensive and sometimes prohibitive. In this study, Latin Hypercube Sampling (LHS) was implemented in a satellite rainfall error model to explore the degree of computational efficiency that could be achieved with a complex hydrologic model. It was found that the LHS method is particularly suited for storms with moderate rainfall. For assessment of errors in time to peak, peak runoff, and runoff volume no significant computational advantage of LHS over the MC method was observed. However, the LHS was able to produce the 80% and higher confidence limits in runoff simulation with the same degree of reliability as MC, but with almost two orders of magnitude fewer simulations. Results from this study indicate that a LHS constrained sampling scheme has the potential to achieve computational efficiency for hydrologic assessment of satellite rainfall retrievals involving: (1) slow running models (such as distributed hydrologic models and land surface models); (2) large study regions; and (3) long study periods; provided the assessment is confined to analysis of the large error bounds of the runoff distribution. (c) 2005 Elsevier Ltd. All rights reserved.
机译:随着2009年全球降水量测量(GPM)的到来,预计卫星降水量测量将以与空缺集水区洪水预报相关的时空尺度在全球范围内可用。为了在洪水预测中对此类取回进行不确定性评估,需要开发可表征卫星取回误差结构的误差模型。全面评估将需要对卫星误差模型实现进行大量的蒙特卡洛(MC)运行,每次都要通过水文模型,以便得出径流中的概率分布。但是,对于慢速运行的水文模型而言,这可能会导致计算量大,有时甚至无法承受。在这项研究中,在卫星降雨误差模型中实施了拉丁超立方采样(LHS),以探索复杂水文模型可以实现的计算效率。人们发现,LHS方法特别适用于降雨量适中的风暴。为了评估峰顶时间,峰径流量和径流量的误差,没有观察到LHS优于MC方法的计算优势。但是,LHS能够在径流模拟中产生80%和更高的置信度极限,并且具有与MC相同的可靠性,但模拟量却减少了近两个数量级。这项研究的结果表明,LHS约束采样方案有可能实现计算卫星降雨取水量的水文评估的计算效率,其中包括:(1)慢速运行模型(例如分布式水文模型和地表模型); (2)研究区域大; (3)学习时间长;如果评估仅限于分析径流分布的大误差范围。 (c)2005 Elsevier Ltd.保留所有权利。

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