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Quantification of predictive uncertainty with a metamodel: toward more efficient hydrologic simulations

机译:利用元模型对预测不确定性进行量化:实现更有效的水文模拟

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摘要

Hydrologic flood prediction has been a quite complex and difficult task because of various sources of inherent uncertainty. Accurately quantifying these uncertainties plays a significant role in providing flood warnings and mitigating risk, but it is time-consuming. To offset the cost of quantifying the uncertainty, we adopted a highly efficient metamodel based on polynomial chaos expansion (PCE) theory and applied it to a lumped, deterministic rainfall-runoff model (NedbOr-AfstrOmnings model, NAM) combined with generalized likelihood uncertainty estimation (GLUE). The central conclusions are: (1) the subjective aspects of GLUE (e.g., the cutoff threshold values of likelihood function) are investigated for 8 flood events that occurred in the Thu bon river watershed in Vietnam, resulting that the values of 0.82 for Nash-Sutcliffe efficiency, 4.05% for peak error, and 4.35% for volume error are determined as the acceptance thresholds. Moreover, the number of ensemble behavioral sets required to maintain the sufficient range of uncertainty but to avoid any unnecessary computation was set to 500. (2) The number of experiment designs (N) and degree of polynomial (p) are key factors in estimating PCE coefficients, and values of N=50 and p=4 are preferred. (3) The results computed using a PCE model consisting of polynomial bases are as good as those given by the NAM, while the total times required for making an ensemble in the PCE model are approximately seventeen times faster. (4) Two parameters (CQOF and CK12) turned out to be most dominant based on a visual inspection of the posterior distribution and the mathematical computations of the Sobol' and Morris sensitivity analysis. Identification of the posterior parameter distributions from the calibration process helps to find the behavioral sets even faster. The unified framework that presents the most efficient ways of predicting flow regime and quantifying the uncertainty without deteriorating accuracy will ultimately be helpful for providing warnings and mitigating flood risk in a timely manner.
机译:由于内在不确定性的各种来源,水文洪水预报一直是一项非常复杂和困难的任务。准确地量化这些不确定性在提供洪水预警和减轻风险方面起着重要作用,但是这很费时。为了抵消量化不确定性的成本,我们采用了基于多项式混沌扩展(PCE)理论的高效元模型,并将其应用于集总,确定性降雨-径流模型(NedbOr-AfstrOmnings模型,NAM)与广义似然不确定性估计的组合(胶)。中心结论是:(1)针对越南Thu bon河流域发生的8次洪水事件,研究了GLUE的主观方面(例如,似然函数的临界阈值),因此Nash-0.82的值Sutcliffe效率,峰误差的4.05%和体积误差的4.35%被确定为接受阈值。而且,为了保持足够的不确定性范围而避免任何不必要的计算所需的总体行为集的数量设置为500。(2)实验设计的数量(N)和多项式的级数(p)是估计的关键因素PCE系数以及N = 50和p = 4的值是优选的。 (3)使用由多项式基数组成的PCE模型计算的结果与NAM给出的结果一样好,而在PCE模型中进行集成所需的总时间大约快了17倍。 (4)根据对后验分布的目视检查以及Sobol'和Morris敏感性分析的数学计算,两个参数(CQOF和CK12)成为最主要的参数。从校准过程中识别后参数分布有助于更快地找到行为集。统一的框架提供了最有效的方法来预测流量变化趋势和量化不确定性,而又不降低准确性,最终将有助于及时提供警告和减轻洪水风险。

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