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Modeling of stationary and non-stationary hydrologic processes.

机译:固定和非固定水文过程的建模。

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This dissertation touches on several aspects related to modeling of stationary and non-stationary hydrologic processes. New methods for regional frequency analysis of extreme events are developed, under the concept of the population index flood (PIF). In this method population quantities are used for estimating the index flood, instead of using the sample mean as is done in traditional index flood methods. PIF models are developed for commonly used distributions in hydrology, and procedures for estimating the standard error of at-site quantile estimators are also developed. Extensive simulation experiments are used to test the proposed methods and procedures based on the PIF models. In addition, a Pareto model is developed utilizing only the largest sample order statistics for parameter estimation based on maximum likelihood, and exact formulas for the mean-squared-error of quantile estimators are also derived. Furthermore, shifting mean models are developed for modeling processes that exhibit a type of non-stationarity in the mean, that is represented by sudden shifting patterns. The shifting mean models are formulated under both univariate and multivariate frameworks, and with and without autoregressive AR(1) persistence. Procedures for parameter estimation are explained in detail. The multivariate model is formulated as a contemporaneous shifting mean model and it is further mixed with contemporaneous ARMA models. That is, the multivariate model is capable of modeling mixed systems, where only part of the sites exhibit sudden shifting patterns and the others sites can be represented by a CARMA( p,q) model. The proposed shifting mean models are capable of preserving key statistical characteristics, and in addition the lag zero spatial correlation in the multivariate models. Numerous examples are presented throughout the dissertation for illustrating the different procedures.
机译:本文涉及与静态和非静态水文过程建模有关的几个方面。在人口指数洪水(PIF)的概念下,开发了用于极端事件的区域频率分析的新方法。在这种方法中,人口数量用于估计指数洪水,而不是像传统的指数洪水方法那样使用样本均值。针对水文中常用的分布开发了PIF模型,还开发了用于估计现场分位数估计器标准误差的程序。大量的仿真实验被用来测试基于PIF模型的方法和程序。此外,仅使用最大样本阶次统计量来开发Pareto模型,以便基于最大似然进行参数估计,并且还得出了分位数估计量的均方误差的精确公式。此外,开发了移动均值模型用于建模过程,该过程表现出均值中的一种非平稳性,这由突然的移动模式表示。移动均值模型是在单变量和多变量框架下制定的,带有和不带有自回归AR(1)持久性。详细说明参数估计的过程。多元模型被表述为同时期均值模型,并与当代ARMA模型进一步混合。也就是说,多元模型能够对混合系统进行建模,其中只有部分位点表现出突然的移位模式,而其他位点可以由CARMA( p,q )模型表示。提出的移动均值模型能够保留关键的统计特征,此外,多元模型中的滞后零空间相关性也是如此。全文中给出了许多例子来说明不同的过程。

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