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首页> 外文期刊>Journal of Hydrology >Regional flood frequency analyses involving extraordinary flood events at ungauged sites: further developments and validations
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Regional flood frequency analyses involving extraordinary flood events at ungauged sites: further developments and validations

机译:区域洪水频率分析,涉及未启用站点的特大洪水事件:进一步的发展和验证

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摘要

Flood frequency analyses are often based on recorded series at gauging stations. However, the length of the available data sets is usually too short to provide reliable estimates of extreme design floods. Hence, hydrologists have tried to make use of alternative sources of information to enrich the datasets used for the statistical inferences. Two main approaches were therefore proposed. The first consists in extending the information in time, making use of historical and paleoflood data. The second, spatial extension, consists in merging statistically homogeneous data to build large regional data samples. Recently, a combination of the two techniques aiming at including estimated extreme discharges at ungauged sites of a region in the regional flood frequency analyses has been proposed. This paper presents a consolidation of this approach and its comparison with the standard regional flood frequency approach proposed by Hosking & Wallis. A modification of the likelihood function is introduced to enable the simultaneous calibration of a regional index flood relation and of the parameters of the regional growth curve. Moreover, the efficiency of the proposed method is evaluated based on a large number of Monte Carlo simulated data sets. This work confirms that extreme peak discharges estimated at ungauged sites may be of great value for the evaluation of large return period (typically over 100 years) flood quantiles. They should therefore not be neglected despite the uncertainties associated to these estimates.
机译:洪水频率分析通常基于测量站的记录序列。但是,可用数据集的长度通常太短,无法提供可靠的极端设计洪水估算。因此,水文学家试图利用替代信息源来丰富用于统计推论的数据集。因此,提出了两种主要方法。首先是利用历史数据和古洪水数据及时扩展信息。第二种是空间扩展,在于合并统计上均一的数据以构建大型区域数据样本。近来,已经提出了两种技术的组合,其旨在在区域洪水频率分析中包括估计的区域的未引流点处的极端排放。本文介绍了该方法的合并方法,并将其与Hosking&Wallis提出的标准区域洪水频率方法进行了比较。引入了对似然函数的修改,以使得能够同时校准区域指数泛滥关系和区域增长曲线的参数。此外,基于大量的蒙特卡洛模拟数据集评估了所提出方法的效率。这项工作证实,在未开垦地点估计的极端洪峰排放量对于评估大洪水期(通常超过100年)洪水分位数可能具有重要价值。因此,尽管这些估计存在不确定性,但不应忽略它们。

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