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新疆木垒县低山区暴雨递减指数分析

Analysis of Rainstorm Decline Index in low mountain Area of Mulei county,Xinjiang autonomous region
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摘要 "推理公式法"作为集总式雨洪模型常用于小流域暴雨洪水计算,暴雨递减指数作为敏感参数对计算成果影响较大。为提高模型计算精度,选用跃进水库入库水文站暴雨资料,分析率定新疆木垒县低山区暴雨递减指数。成果显示该区域暴雨递减指数随频率的增大而减小,随时段的增大而增大,以1h为界,n1在0.163―0.330之间,n2在0.597―0.764之间。分析成果可供周边设计暴雨计算及雨洪模型使用。 "inferential formula method",as a lump-sum rainstorm flood model,is often used in the calculation of rainstorm flood in small watershed.In order to improve the accuracy of the model calculation,the rainstorm data of yuejin reservoir storage station was selected to determine the rainstorm decline index of low mountain area in mushi county of xinjiang at an analysis rate.The results show that the rainstorm decline index in this region decreases with the increase of frequency,and increases with the increase of the time interval.It is bounded by 1 h,n1 is between 0.163 and 0.330,and n2 is between 0.597 and 0.764.The analysis results can be used for peripheral design storm calculation and flood model.
作者 赵宏涛 Zhao Hong-tao
出处 《吉林水利》 2018年第8期55-57,62,共4页 Jilin Water Resources
关键词 木垒县 低山区 暴雨递减指数 Mulei county Low mountains Rainstorm decline index
作者简介 赵宏涛(1985-),男,汉,河南舞阳人,学士,工程师,从事水利水电勘察设计。
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