大渡河流域超阈值降雨样本模拟及不确定性分析  

Simulation of above-threshold rainfall sample series of Dadu River Basin and uncertainty analysis

作　　者：鲁帆[1] 宋昕熠 朱奎[2] 陈争杰 

机构地区：[1]中国水利水电科学研究院水资源研究所,北京100038 [2]中国矿业大学资源与地球科学学院,江苏徐州221116

出　　处：《人民长江》2016年第7期23-27,33,共6页Yangtze River

基　　金：国家重点基础研究发展"973"计划项目"梯级水库群风险预警与应急处置机理"(2013CB036406);国家自然科学基金项目"风险规避视角下跨流域调水工程可调水量概率预报的基础研究"(51109224)

摘　　要：大渡河流域地形十分复杂,流域内气候随高程变化差异较大。通过超阈值模型模拟大渡河流域范围内9个雨量站的逐日降水资料序列,利用极大似然估计法计算模型参数,采用概率图、分位数图、重现水平图、密度函数图4种较直观的诊断图形对模型的合理性进行了全面评估,并借助轮廓似然方法估计模型关键参数及设计强降雨的置信区间。研究结果表明,各站点超阈值降雨样本均服从Pareto分布,可以选择GPD模型作为大渡河流域强降雨统计推断的分布函数类型,轮廓似然法能反映重现期长短对设计降雨置信区间的影响。可为大渡河流域降雨不确定性的定量评估及梯级水库群洪水预报提供依据。The topography of Dadu River Basin is complicated,and its climate has a comparatively large difference with the elevation variation.Above-threshold model is used to fit the daily rainfall samples of nine rainfall stations in Dadu River Basin,based on this,the parameters of the model are estimated by maximum likelihood method and the fitting results are tested by probability plot,quantile plot,return level plot and density plot.Moreover,the profile likelihood function was used to estimate the key parameters of the model and the confidence interval of designed heavy rainfall.The results indicate that above-threshold precipitation samples of the 9 stations follow the Pareto distribution.The GPD model can be selected as the distribution function type of statistics inference of rainfall of Dadu River Basin.The Profile likelihood function method can reflect the effect of the length of return periods on confidence interval.The methods and results can help analyzing the uncertainty of extreme values of rainfall and flood forecast of cascade reservoirs of Dadu River Basin.

关 键 词：GPD模型 轮廓似然函数 不确定性 大渡河 

分 类 号：P33[天文地球—水文科学]