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首页> 外文期刊>Theoretical and applied climatology >Bivariate hydrologic risk analysis based on a coupled entropy-copula method for the Xiangxi River in the Three Gorges Reservoir area, China
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Bivariate hydrologic risk analysis based on a coupled entropy-copula method for the Xiangxi River in the Three Gorges Reservoir area, China

机译:基于三峡库的湘西河水文风险分析

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摘要

In this study, a bivariate hydrologic risk framework is proposed based on a coupled entropy-copula method. In the proposed risk analysis framework, bivariate flood frequency would be analyzed for different flood variable pairs (i.e., flood peak-volume, flood peak-duration, flood volume-duration). The marginal distributions of flood peak, volume, and duration are quantified through both parametric (i.e., gamma, general extreme value (GEV), and lognormal distributions) and nonparametric (i.e., entropy) approaches. The joint probabilities of flood peak-volume, peak-duration, and volume-duration are established through copulas. The bivariate hydrologic risk is then derived based on the joint return period to reflect the interactive effects of flood variables on the final hydrologic risk values. The proposed method is applied to the risk analysis for the Xiangxi River in the Three Gorges Reservoir area, China. The results indicate the entropy method performs best in quantifying the distribution of flood duration. Bivariate hydrologic risk would then be generated to characterize the impacts of flood volume and duration on the occurrence of a flood. The results suggest that the bivariate risk for flood peak-volume would not decrease significantly for the flood volume less than 1000 m(3)/s. Moreover, a flood in the Xiangxi River may last at least 5 days without significant decrease of the bivariate risk for flood peak-duration.
机译:在这项研究中,提出了基于耦合熵-copula方法的双变量水文风险框架。在建议的风险分析框架中,将针对不同的洪水变量对(即洪水峰量,洪水峰持续时间,洪水量持续时间)分析双变量洪水频率。洪水峰,流量和持续时间的边际分布通过参数(即伽马,一般极值(GEV)和对数正态分布)和非参数(即熵)方法进行量化。通过copulas确定洪水峰量,峰持续时间和体积持续时间的联合概率。然后根据联合返回期推算出双变量水文风险,以反映洪水变量对最终水文风险值的相互作用。该方法应用于三峡库区湘西河的风险分析。结果表明,熵方法在量化洪水持续时间的分布方面表现最佳。然后将产生双变量水文风险,以表征洪水量和持续时间对洪水发生的影响。结果表明,当洪水量小于1000 m(3)/ s时,洪水高峰量的二元风险不会显着降低。而且,湘西河的洪灾可能至少持续5天,而洪峰持续时间的二元风险没有显着降低。

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  • 来源
    《Theoretical and applied climatology》 |2016年第2期|381-397|共17页
  • 作者单位

    Univ Regina, Fac Engn & Appl Sci, Regina, SK S4S 0A2, Canada;

    McMaster Univ, Dept Civil Engn, Hamilton, ON L8S 4L8, Canada;

    Univ Regina, Inst Energy Environm & Sustainabil Res, UR NCEPU, Regina, SK S4S 0A2, Canada|North China Elect Power Univ, MOE Key Lab Reg Energy & Environm Syst Optimizat, Beijing 102206, Peoples R China;

    Univ Regina, Fac Engn & Appl Sci, Regina, SK S4S 0A2, Canada;

    North China Elect Power Univ, MOE Key Lab Reg Energy & Environm Syst Optimizat, Beijing 102206, Peoples R China;

    North China Elect Power Univ, MOE Key Lab Reg Energy & Environm Syst Optimizat, Beijing 102206, Peoples R China;

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