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高玉琴, 叶 柳, 赖丽娟.基于G-H copula函数的秦淮河流域洪水风险分析水资源与水工程学报[J].,2018,29(1):172-177
基于G-H copula函数的秦淮河流域洪水风险分析
Analysis of flood risk in Qinhuai River Basin based on G-H copula
  
DOI:10.11705/j.issn.1672-643X.2018.01.29
中文关键词:  洪水风险分析  超越概率  Kendall重现期  联合重现期  秦淮河流域
英文关键词:flood risk analysis  exceedance probability  Kendall return period  joint return period  Qinhuai river basin
基金项目:国家自然科学基金青年项目(51309076); 中央高校基金前瞻性项目(2014B05814); 江苏省优势创新平台项目
作者单位
高玉琴, 叶 柳, 赖丽娟 (河海大学 水利水电学院 江苏 南京 210098) 
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中文摘要:
      Copula函数构造灵活,适应性强,被广泛应用于多变量水文频率分析计算中。选取G-H copula函数描述洪量、洪峰、洪水位间的相依结构,边际分布模拟考虑广义极值(GEV),对数正态(ln2)和皮尔逊Ⅲ型分布(P-Ⅲ)。以相关性最强的洪峰和洪水位为例进行二维变量洪水风险分析,比较分析其传统重现期和Kendall重现期性质,并计算条件风险率。构建3变量联合风险评价模型,并与二变量情况进行对比。以秦淮河流域为例进行了应用,表明多维联合重现期小于同现重现期,Kendall重现期在两者之间且与单因素重现期误差最小;流域洪峰和洪水位同现风险率最大,洪峰量级越小,洪水位超越风险率越小;基于三维G-H copula函数计算的各变量同频率设计值大于相应单变量设计值,并且相对于二维情况,各重现期与单因素重现期之间的差值明显增大。研究结论可为秦淮河地区水利工程规划设计和洪灾风险评估提供有益参考。
英文摘要:
      Copula function is commonly used in the flood frequency calculation of multidimensional variables because of its flexible construction and wide adaptability. G-H copula is selected to describe the dependence structure of three flood variables, namely flood volume, peak flow and water level. GEV, Logical-normal and PearsonⅢ distribution are considered for fitting the marginal distribution. A two-dimensional G-H copula flood risk assessment model based on peak flow and water level, which are of the highest dependence, is developed to investigate and analyze the characteristics of joint return period (JRP), co-recurrence return period and Kendall return period (KRP). The conditional risk of different combination of flood events is also computed. A three-dimensional G-H copula model is also developed to compare with the bivariate scenario. Qinhuai river basin is chosen as the study area. The result shows that the multi-dimensional joint return period is quite smaller than the co-recurrence return period. Kendall return period is in between of joint and co-recurrence return period but has the minimum error with the single variable return period. The co-recurrence probability of peak flow and water level turns out to be the highest; the smaller the magnitude of peak flow, the less possible for water level to exceed certain threshold. The design value of flood variables in same frequency computed by trivariate G-H copula is larger than the corresponding single variable design value and the difference of other return period with single variable return period is obviously larger than that of bivariate case. The conclusion can be useful for water resource project planning and design and risk assessment of flood disaster in the studied area.
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