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首页> 外文期刊>Hydrology and Earth System Sciences >The transformed-stationary approach: a generic and simplified methodology for non-stationary extreme value analysis
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The transformed-stationary approach: a generic and simplified methodology for non-stationary extreme value analysis

机译:平稳转化方法:非平稳极值分析的通用简化方法

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Statistical approaches to study extreme events require, by definition, long time series of data. In many scientific disciplines, these series are often subject to variations at different temporal scales that affect the frequency and intensity of their extremes. Therefore, the assumption of stationarity is violated and alternative methods to conventional stationary extreme value analysis?(EVA) must be adopted. Using the example of environmental variables subject to climate change, in this study we introduce the transformed-stationary?(TS) methodology for non-stationary EVA. This approach consists of (i)?transforming a non-stationary time series into a stationary one, to which the stationary EVA theory can be applied, and (ii)?reverse transforming the result into a non-stationary extreme value distribution. As a transformation, we propose and discuss a simple time-varying normalization of the signal and show that it enables a comprehensive formulation of non-stationary generalized extreme value?(GEV) and generalized Pareto distribution?(GPD) models with a constant shape parameter. A validation of the methodology is carried out on time series of significant wave height, residual water level, and river discharge, which show varying degrees of long-term and seasonal variability. The results from the proposed approach are comparable with the results from (a)?a stationary EVA on quasi-stationary slices of non-stationary series and (b)?the established method for non-stationary EVA. However, the proposed technique comes with advantages in both cases. For example, in contrast to?(a), the proposed technique uses the whole time horizon of the series for the estimation of the extremes, allowing for a more accurate estimation of large return levels. Furthermore, with respect to?(b), it decouples the detection of non-stationary patterns from the fitting of the extreme value distribution. As a result, the steps of the analysis are simplified and intermediate diagnostics are possible. In particular, the transformation can be carried out by means of simple statistical techniques such as low-pass filters based on the running mean and the standard deviation, and the fitting procedure is a stationary one with a few degrees of freedom and is easy to implement and control. An open-source MATLAB toolbox has been developed to cover this methodology, which is available at a href="https://github.com/menta78/tsEva/" target="_blank"https://github.com/menta78/tsEva//a (Mentaschi et al.,?2016).
机译:根据定义,研究极端事件的统计方法需要长时间的数据序列。在许多科学学科中,这些序列经常会在不同的时间尺度上变化,从而影响其极端事件的频率和强度。因此,违反了平稳性的假设,必须采用常规平稳极值分析(EVA)的替代方法。使用受气候变化影响的环境变量的示例,在本研究中,我们介绍了用于非平稳EVA的转化平稳(TS)方法。此方法包括(i)将非平稳时间序列转换为平稳的时间序列,可以应用平稳EVA理论,以及(ii)将结果反向转换为非平稳的极值分布。作为一种变换,我们提出并讨论了一种简单的信号时变归一化方法,并表明它可以对具有固定形状参数的非平稳广义极值(GEV)模型和广义Pareto分布(GPD)模型进行综合表示。 。该方法论的验证是在重要波高,残留水位和河流流量的时间序列上进行的,这些时间序列显示出不同程度的长期和季节性变化。所提出的方法的结果与(a)非平稳序列的准平稳切片上的固定EVA和(b)非平稳EVA的既定方法的结果可比。但是,所提出的技术在两种情况下都具有优势。例如,与?(a)相反,所提出的技术将序列的整个时间范围用于极端值的估计,从而可以更准确地估计大收益水平。此外,关于β(b),它使非平稳模式的检测与极值分布的拟合解耦。结果,简化了分析步骤,并且可以进行中间诊断。尤其是,可以通过简单的统计技术(例如基于运行平均值和标准偏差的低通滤波器)进行转换,并且拟合过程是具有几个自由度的固定过程,易于实现和控制。已经开发了涵盖此方法的开源MATLAB工具箱,该工具箱可从href="https://github.com/menta78/tsEva/" target="_blank"> https://github.com/获得。 menta78 / tsEva / (Mentaschi et al。,?2016)。

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