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首页> 外文期刊>Hydrology and Earth System Sciences >Non-stationary flood frequency analysis in continental Spanish rivers, using climate and reservoir indices as external covariates
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Non-stationary flood frequency analysis in continental Spanish rivers, using climate and reservoir indices as external covariates

机译:使用气候和水库指数作为外部协变量的西班牙大陆河流非平稳洪水频率分析

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摘要

Recent evidences of the impact of persistent modes ofregional climate variability, coupled with the intensification of humanactivities, have led hydrologists to study flood regime without applying thehypothesis of stationarity. In this study, a framework for flood frequencyanalysis is developed on the basis of a tool that enables us to address themodelling of non-stationary time series, namely, the "generalized additivemodels for location, scale and shape" (GAMLSS). Two approaches tonon-stationary modelling in GAMLSS were applied to the annual maximum floodrecords of 20 continental Spanish rivers. The results of the first approach,in which the parameters of the selected distributions were modelled as afunction of time only, show the presence of clear non-stationarities in theflood regime. In a second approach, the parameters of the flooddistributions are modelled as functions of climate indices (ArcticOscillation, North Atlantic Oscillation, Mediterranean Oscillation and theWestern Mediterranean Oscillation) and a reservoir index that is proposed inthis paper. The results when incorporating external covariates in the studyhighlight the important role of interannual variability in low-frequencyclimate forcings when modelling the flood regime in continental Spanishrivers. Also, with this approach it is possible to properly introduce theimpact on the flood regime of intensified reservoir regulation strategies.The inclusion of external covariates permits the use of these models aspredictive tools. Finally, the application of non-stationary analysis showsthat the differences between the non-stationary quantiles and theirstationary equivalents may be important over long periods of time.
机译:持续的区域气候变化模式的影响的最新证据,再加上人类活动的加剧,促使水文学家在不采用平稳假说的情况下研究洪水状况。在本研究中,在一种工具的基础上开发了洪水频率分析框架,该工具使我们能够解决非平稳时间序列的建模问题,即“位置,尺度和形状的通用加性模型”(GAMLSS)。 GAMLSS中的两种非平稳建模方法已应用于20条西班牙大陆河流的年度最大洪水记录。第一种方法的结果(其中所选分布的参数仅被建模为时间的函数)表明,在洪水状态中存在明显的非平稳性。在第二种方法中,将洪水分布的参数建模为气候指数(ArcticOscillation,北大西洋涛动,地中海涛动和西地中海涛动)和本文提出的水库指数的函数。在将外部协变量纳入研究中的结果强调了在模拟西班牙大陆河的洪水方式时,年际变化在低频气候强迫中的重要作用。同样,通过这种方法,有可能适当地引入对强化水库调节策略的洪水影响。外部协变量的包含允许使用这些模型作为预测工具。最后,非平稳分析的应用表明,非平稳分位数及其平稳等价物之间的差异可能在很长一段时间内很重要。

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