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SCALE MIXTURES OF FRECHET DISTRIBUTIONS AS ASYMPTOTIC APPROXIMATIONS OF EXTREME PRECIPITATION

机译:频率分布的混合,作为极端降水的渐近逼近

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摘要

This paper is a further development of the results of [20] where, based on the negative binomial model for the duration of wet periods measured in days [16], an asymptotic approximation was proposed for the distribution of the maximum daily precipitation volume within a wet period. This approximation has the form of a scale mixture of the Fr´echet distribution with the gamma mixing distribution and coincides with the distribution of a positive power of a random variable having the Snedecor–Fisher distribution. Here we extend this result to the m th extremes, m  ∈  ℕ , and sample quantiles. The proof of this result is based on the representation of the negative binomial distribution as a mixed geometric (and hence, mixed Poisson) distribution [17] and limit theorems for extreme order statistics in samples with random sizes having mixed Poisson distributions [10]. Some analytic properties of the obtained limit distribution are described. In particular, it is demonstrated that under certain conditions the limit distribution of the maximum precipitation is mixed exponential and hence, is infinitely divisible. It is shown that under the same conditions this limit distribution can be represented as a scale mixture of stable or Weibull or Pareto or folded normal laws. The corresponding product representations for the limit random variable can be used for its computer simulation. The results of fitting this distribution to real data are presented illustrating high adequacy of the proposed model. It is also shown that the limit distribution of sample quantiles is the well-known Student distribution. Several methods are proposed for the estimation of the parameters of the asymptotic distributions. The obtained mixture representations for the limit laws and the corresponding asymptotic approximations provide better insight into the nature of mixed probability (“Bayesian”) models.
机译:本文是对[20]的结果的进一步发展,其中基于负二项式模型对以天为单位的潮湿时段的持续时间[16]提出了一种渐近逼近法,用于计算最大日降水量在一个区域内的分布。湿期。这种近似具有Fr'echet分布和γ混合分布的比例混合形式,并且与具有Snedecor-Fisher分布的随机变量的正幂分布一致。在这里,我们将此结果扩展到第m个极点m∈and,并采样分位数。该结果的证明是基于负二项分布作为混合几何(因此也就是混合泊松)分布的表示[17],并针对具有混合泊松分布的随机大小的样本中极限顺序统计的极限定理[10]。描述了获得的极限分布的一些解析性质。特别地,证明了在某些条件下最大降水的极限分布是混合指数的,因此可以无限地整除。结果表明,在相同条件下,该极限分布可以表示为稳定或威布尔或帕累托或折叠正态定律的比例混合。极限随机变量的相应产品表示形式可用于其计算机仿真。给出了使这种分布适合实际数据的结果,说明了所提出模型的高度充分性。还表明样本分位数的极限分布是众所周知的学生分布。提出了几种估计渐近分布参数的方法。所获得的极限定律的混合表示以及相应的渐近逼近可更好地了解混合概率(“贝叶斯”)模型的性质。

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  • 来源
    《Journal of Mathematical Sciences》 |2018年第6期|886-903|共18页
  • 作者单位

    Lomonosov Moscow State University, Faculty of Computational Mathematics and Cybernetics,Institute of Informatics Problems, Federal Research Center “Computer Science and Control” of the Russian Academy of Sciences;

    Lomonosov Moscow State University, Faculty of Computational Mathematics and Cybernetics,Institute of Informatics Problems, Federal Research Center “Computer Science and Control” of the Russian Academy of Sciences;

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