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Characterization of process-oriented hydrologic model behavior with temporal sensitivity analysis for flash floods in Mediterranean catchments

机译:地中海流域突发性洪水过程敏感性的时间敏感性分析

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This paper presents a detailed analysis of 10 flash flood events in the Mediterranean region using the distributed hydrological model MARINE. Characterizing catchment response during flash flood events may provide new and valuable insight into the dynamics involved for extreme catchment response and their dependency on physiographic properties and flood severity. The main objective of this study is to analyze flash-flood-dedicated hydrologic model sensitivity with a new approach in hydrology, allowing model outputs variance decomposition for temporal patterns of parameter sensitivity analysis. Such approaches enable ranking of uncertainty sources for nonlinear and nonmonotonic mappings with a low computational cost. Hydrologic model and sensitivity analysis are used as learning tools on a large flash flood dataset. With Nash performances above 0.73 on average for this extended set of 10 validation events, the five sensitive parameters of MARINE process-oriented distributed model are analyzed. This contribution shows that soil depth explains more than 80% of model output variance when most hydrographs are peaking. Moreover, the lateral subsurface transfer is responsible for 80% of model variance for some catchment-flood events' hydrographs during slow-declining limbs. The unexplained variance of model output representing interactions between parameters reveals to be very low during modeled flood peaks and informs that model-parsimonious parameterization is appropriate to tackle the problem of flash floods. Interactions observed after model initialization or rainfall intensity peaks incite to improve water partition representation between flow components and initialization itself. This paper gives a practical framework for application of this method to other models, landscapes and climatic conditions, potentially helping to improve processes understanding and representation.
机译:本文使用分布式水文模型MARINE对地中海地区的10次暴洪事件进行了详细分析。在山洪暴发事件期间表征集水区响应,可以为涉及极端集水区响应及其对地物特征和洪水严重性的依赖性的动力学提供新的有价值的见解。这项研究的主要目的是使用一种新的水文学方法来分析洪水专用水文模型的敏感性,从而允许模型输出方差分解以进行参数敏感性分析的时间模式。这样的方法能够以低的计算成本对非线性和非单调映射的不确定性源进行排序。水文模型和敏感性分析被用作大型山洪数据集的学习工具。对于这套扩展的10个验证事件,Nash平均性能高于0.73,分析了面向MARINE过程的分布式模型的五个敏感参数。这一贡献表明,当大多数水位图达到峰值时,土壤深度解释了模型输出差异的80%以上。此外,在缓慢下降的肢体中,对于某些集水洪水事件的水文图,横向地下地下移移是模型方差的80%。代表参数之间相互作用的模型输出的无法解释的方差显示,在建模洪峰期间非常低,这表明模型简约的参数化适合解决山洪泛滥的问题。在模型初始化或降雨强度峰值之后观察到的相互作用促进了流量分量和初始化本身之间的水分配表示。本文为将该方法应用于其他模型,景观和气候条件提供了一个实用的框架,可能有助于提高对过程的理解和表示。

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