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On the asymptotic behavior of flood peak distributions

机译:洪峰分布的渐近行为

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This paper presents some analytical results and numerical illustrations on the asymptotic properties of flood peak distributions obtained through derived flood frequency approaches. It confirms and extends the results of previous works: i.e. the shape of the flood peak distributions are asymptotically controlled by the rainfall statistical properties, given limited and reasonable assumptions concerning the rainfall-runoff process. This result is partial so far: the impact of the rainfall spatial heterogeneity has not been studied for instance. From a practical point of view, it provides a general framework for analysis of the outcomes of previous works based on derived flood frequency approaches and leads to some proposals for the estimation of very large return-period flood quantiles. This paper, focussed on asymptotic distribution properties, does not propose any new approach for the extrapolation of flood frequency distribution to estimate intermediate return period flood quantiles. Nevertheless, the large distance between frequent flood peak values and the asymptotic values as well as the simulations conducted in this paper help quantifying the ill condition of the problem of flood frequency distribution extrapolation: it illustrates how large the range of possibilities for the shapes of flood peak distributions is.
机译:本文介绍了一些通过导出洪水频率方法获得的洪水峰值分布的渐近性质的分析结果和数值例证。它证实并扩展了先前工作的结果:即,在有关降雨径流过程的假设有限且合理的前提下,洪水峰值分布的形状由降雨统计特性渐进控制。到目前为止,这一结果是不完整的:例如,尚未研究降雨空间异质性的影响。从实践的角度来看,它为基于派生洪水频率方法的先前工作成果的分析提供了一个通用框架,并为估算非常大的回水期洪水分位数提出了一些建议。本文着眼于渐近分布特性,没有提出任何新的方法来外推洪水频率分布以估算中间返回期洪水位数。尽管如此,频繁洪水峰值和渐近值之间的较大距离以及本文进行的模拟仍有助于量化洪水频率分布外推问题的病态:它说明了洪水形状的可能性范围有多大峰分布是。

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