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Probability distribution of flood flows in Tunisia

机译:突尼斯洪水流量的概率分布

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摘要

L (Linear) moments are used in identifying regional flood frequency distributions for different zones Tunisia wide. 1134 site-years of annual maximum stream flow data from a total of 42 stations with an average record length of 27 years are considered. The country is divided into two homogeneous regions (northern and central/southern Tunisia) using a heterogeneity measure, based on the spread of the sample L-moments among the sites in a given region. Then, selection of the corresponding distribution is achieved through goodness-of-fit comparisons in L-moment diagrams and verified using an L moment based regional test that compares observed to theoretical values of L-skewness and L-kurtosis for various candidate distributions. The distributions used, which represent five of the most frequently used distributions in the analysis of hydrologic extreme variables are: (i) Generalized Extreme Value (GEV), (ii) Pearson Type III (P3), (iii) Generalized Logistic (GLO), (iv) Generalized Normal (GN), and (v) Generalized Pareto (GPA) distributions. Spatial trends, with respect to the best-fit flood frequency distribution, are distinguished: Northern Tunisia was shown to be represented by the GNO distribution while the GNO and GEV distributions give the best fit in central/southern Tunisia.
机译:L(线性)矩用于识别突尼斯全地区不同区域的区域洪水频率分布。考虑了来自总共42个站的平均最大记录长度为27年的1134个站点年度年度最大流量数据。根据样本L矩在给定区域内站点之间的分布,使用异质性度量将该国家分为两个同质区域(北突尼斯和突尼斯中部/南部)。然后,通过在L矩图中进行拟合优度比较来实现对相应分布的选择,并使用基于L矩的区域检验进行验证,该检验将观察到的L偏度和L峰度的理论值与各种候选分布进行比较。所使用的分布代表着水文极端变量分析中五个最常用的分布:(i)广义极值(GEV),(ii)皮尔逊类型III(P3),(iii)广义逻辑(GLO) ,(iv)广义正态(GN)和(v)广义帕累托(GPA)分布。就最合适的洪水频率分布而言,空间趋势有所不同:突尼斯北部以GNO分布为代表,而GNO和GEV分布最适合突尼斯中部/南部。

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