王家祁, 姚惠明, 关铁生. 暴雨和降水偏态系数分析[J]. 水科学进展, 2006, 17(3): 365-370.
引用本文: 王家祁, 姚惠明, 关铁生. 暴雨和降水偏态系数分析[J]. 水科学进展, 2006, 17(3): 365-370.
WANG Jia-qi, YAO Hui-ming, GUAN Tie-sheng. Analysis of skewness coefficient of rainstorm and precipitation[J]. Advances in Water Science, 2006, 17(3): 365-370.
Citation: WANG Jia-qi, YAO Hui-ming, GUAN Tie-sheng. Analysis of skewness coefficient of rainstorm and precipitation[J]. Advances in Water Science, 2006, 17(3): 365-370.

暴雨和降水偏态系数分析

Analysis of skewness coefficient of rainstorm and precipitation

  • 摘要: 采用统一的统计参数计算方法分析计算了全国0.51万~1.36万个雨量站历时为10 min~3 d的暴雨资料、210个站历时为1 d~90 d和1 a的降水资料的偏态系数和变差系数比值Rsv。探讨了皮尔逊Ⅲ型频率分布曲线的Rsv特性;分析了Rsv的地域分布、Rsv与雨量历时的关系,并研究了对Rsv有影响的多个因子。研究表明,在目前资料条件下,不宜对各个地区各种历时的暴雨频率分析均采用单一的Rsv值(3.5)。

     

    Abstract: The ratio of the skewness coefficient to the variation coefficient is computed with uniform method for the rainfall data from 5 100-13 600 stations with durations of 10-min-3-day and 210 stations with durations of 1-day-90-day and 1-year.The ratio of skewness to variation (Rsv) characteristics of the Pearson type Ⅲ frequency distribution are approached; the regional distribution of Rsv and the Rsv-duration relation are analyzed,and the same affected factors on Rsv are studied.On the condition of the data at present,the single Rsv value of 3.5 is not suitable for each region and each duration in rainstorm frequency analyses.

     

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