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Application of Regional Flood Frequency Analysis Based on L-moments in the Region of the Middle and Lower Yangtze River

机译:基于L矩的区域洪水频率分析在长江中下游地区的应用

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摘要

The regional flood frequency analysis method based on L-moments proposed by Hosking in 1997 is applied to the flood frequency analysis of annual maximum flood volume for five hydrological stations ,including Yichang , Shashi, Hankou, Luoshan and Datong , in the middle and lower reaches of Yangtze river. The method of Hosking is a new one for Chinese traditional regional flood frequency analysis. The calculated results shows that the five stations could be considered as an homogenous region for frequency analysis, so the index-flood method is used to calculated design values for each station, and the Wakeby distribution is recommended to be population grow-curve (or distribution),because the other distribution, i.e., Pearson-III,GLO,GEV,GPA, and GLN are not accepted by the Z statistic test
机译:霍斯金(Hosking)在1997年提出的基于L矩的区域洪水频率分析方法被应用于中下游宜昌,沙市,汉口,洛山和大同五个水文站年最大洪水量的洪水频率分析。长江。 Hosking方法是一种用于中国传统区域洪水频率分析的新方法。计算结果表明,可以将这五个站点视为频率分析的同质区域,因此使用指数洪水法来计算每个站点的设计值,并且建议将Wakeby分布设为人口增长曲线(或分布) ),因为Z统计量检验不接受其他分布,即Pearson-III,GLO,GEV,GPA和GLN

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