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Estimation of synthetic flood design hydrographs using a distributed rainfall–runoff model coupled with a copula-based single storm rainfall generator

机译:使用分布式降雨径流模型估算合成泛洪设计文文射程与Copula的单风暴降雨发电机

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In this paper a procedure to derive synthetic flood design hydrographs (SFDH) using a bivariate representation of rainfall forcing (rainfall duration and intensity) via copulas, which describes and models the correlation between two variables independently of the marginal laws involved, coupled with a distributed rainfall–runoff model, is presented. Rainfall–runoff modelling (R–R modelling) for estimating the hydrological response at the outlet of a catchment was performed by using a conceptual fully distributed procedure based on the Soil Conservation Service – Curve Number method as an excess rainfall model and on a distributed unit hydrograph with climatic dependencies for the flow routing. Travel time computation, based on the distributed unit hydrograph definition, was performed by implementing a procedure based on flow paths, determined from a digital elevation model (DEM) and roughness parameters obtained from distributed geographical information. In order to estimate the primary return period of the SFDH, which provides the probability of occurrence of a hydrograph flood, peaks and flow volumes obtained through R–R modelling were treated statistically using copulas. Finally, the shapes of hydrographs have been generated on the basis of historically significant flood events, via cluster analysis. An application of the procedure described above has been carried out and results presented for the case study of the Imera catchment in Sicily, Italy.
机译:在本文中,通过Copulas使用二棱镜代表(降雨持续时间和强度)的二偏角表示,通过Copulas获得合成泛洪设计文化照片(SFDH)的程序,该分组描述和模拟了两个变量与所涉及的边际法律之间的相关性,与分布式相结合提出了降雨径流模型。通过使用基于土壤保护服务 - 曲线数法作为多余的降雨模型和分布式单元,通过使用基于土壤保护服务曲线数法和分布式单元的概念性完全分布的程序来估算集流体出口的水文响应的降雨径流模拟(R-R模型)与流动路由的气候依赖性的水文。通过从基于流路径的过程来执行从分布式单元水文编程定义进行的旅行时间计算通过从分布式地理信息获得的数字高度模型(DEM)和粗糙度参数确定。为了估计SFDH的主要返回时期,该归零期能够出现发生水电图的概率,通过R-R模型获得的峰值和流量进行统计使用Copulas治疗。最后,通过集群分析,在历史上大量的洪水事件的基础上产生了水文的形状。已经进行了上述程序的应用,并且在意大利西西里岛的IMERA集水区呈现和结果。

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