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Modeling of stationary and non-stationary hydrologic processes

dc.contributor.authorSveinsson, Óli Grétar Blöndal, author
dc.contributor.authorSalas, Jose D., advisor
dc.contributor.authorBoes, Duane C., advisor
dc.contributor.authorPielke, Roger A., committee member
dc.contributor.authorRamirez, Jorge A., committee member
dc.date.accessioned2026-01-23T17:29:58Z
dc.date.issued2002
dc.description.abstractThis 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 param eter 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,g) 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.
dc.format.mediumborn digital
dc.format.mediumdoctoral dissertations
dc.identifierETDF_2002_Sveinsson_3053454.pdf
dc.identifier.urihttps://hdl.handle.net/10217/242902
dc.identifier.urihttps://doi.org/10.25675/3.025759
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Libraries
dc.relation.ispartof2000-2019
dc.rightsCopyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.
dc.rights.licensePer the terms of a contractual agreement, all use of this item is limited to the non-commercial use of Colorado State University and its authorized users.
dc.subjecthydrology
dc.subjectcivil engineering
dc.subjecthydrologic sciences
dc.titleModeling of stationary and non-stationary hydrologic processes
dc.typeText
dcterms.rights.dplaThis Item is protected by copyright and/or related rights (https://rightsstatements.org/vocab/InC/1.0/). You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).
thesis.degree.disciplineCivil Engineering
thesis.degree.grantorColorado State University
thesis.degree.levelDoctoral
thesis.degree.nameDoctor of Philosophy (Ph.D.)

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