有界逆威布尔分布:应用于环境最大值的极值替代方案?

Earl Bardsley , Varvara Vetrova
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引用次数: 0

摘要

长期以来,人们一直对推断未来的低概率自然事件感兴趣,这些事件的量级大于过去的任何记录。给定一个平稳的时间序列,无界的1型和2型渐近极值分布通常被用来为水文变量(如降雨和河流流量)的大幅度和长回归期外推提供理论依据。然而,存在一个问题,即极端环境受到其因果变量的有限性的限制。因此,使用无界渐近模型的外推不能从极值理论中得到证明,并且在某些时候会对未来的震级进行过度预测。这就造成了明显的矛盾,例如,尽管降雨量的有限性,但第2类极值分布很好地近似了年降雨量最大值。为了进一步研究,提出了另一种渐近极值方法,该模型是最小值的渐近分布(威布尔分布)应用于阻塞最大倒数。给出了两个例子,其中与类型1或类型2极值分布很好匹配的数据给出了暗示下界的倒数(原始数据的上界γ)。这里的渐近模型是一个往复的3参数威布尔分布,具有正的位置参数γ−1。当这种情况从数据上得到证明时,就可以对3参数威布尔随机变量的倒数分布进行参数估计。这个分布在这里被称为有界逆威布尔分布。提出了一种极大似然参数估计方法,以及一种参数自举方法,用于获得γ的单侧上置信限。当数据允许估计γ时,有界逆威布尔分布被建议作为1型或2型极值分布的改进替代方案,因为上界现实被识别。然而,需要对许多数据集进行广泛的应用,以评估有界方法在最大记录事件外推方面的实际效用。
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The bounded inverse Weibull distribution: An extreme value alternative for application to environmental maxima?

There has long been interest in making inferences about future low-probability natural events that have magnitudes greater than any in the past record. Given a stationary time series, the unbounded Type 1 and Type 2 asymptotic extreme value distributions are often invoked as giving theoretical justification for extrapolating to large magnitudes and long return periods for hydrological variables such as rainfall and river discharge. However, there is a problem in that environmental extremes are bounded above by the bounded nature of their causal variables. Extrapolation using unbounded asymptotic models therefore cannot be justified from extreme value theory and at some point there will be over-prediction of future magnitudes. This creates the apparent contradiction, for example, of annual rainfall maxima being well approximated by Type 2 extreme value distributions despite the bounded nature of rainfall magnitudes. An alternative asymptotic extreme value approach is suggested for further investigation, with the model being the asymptotic distribution of minima (Weibull distribution) applied to block maxima reciprocals. Two examples are presented where data that are well matched by Type 1 or Type 2 extreme value distributions give reciprocals suggestive of lower bounds (upper bound γ to the original data). The asymptotic model here is a 3-parameter Weibull distribution for the reciprocals, with positive location parameter γ−1. When this situation is demonstrated from data, parameter estimation can be carried out with respect to the distribution of reciprocals of 3-parameter Weibull random variables. This distribution is referenced here as the bounded inverse Weibull distribution. A maximum likelihood parameter estimation methodology is presented, together with a parametric bootstrap approach for obtaining one-sided upper confidence limits to γ. When data permits estimation of γ, the bounded inverse Weibull distribution is suggested as an improved alternative to Type 1 or Type 2 extreme value distributions because the upper bound reality is recognised. However, extensive application to many data sets is required to evaluate the practical utility of the bounded approach for extrapolating beyond the largest recorded event.

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