EFFECT OF THE OCCURRENCE PROCESS OF THE PEAKS OVER THRESHOLD ON THE FLOOD ESTIMATES

dc.contributor.authorOnoz B.
dc.contributor.authorBayazit M.
dc.date.accessioned2021-02-11T07:53:53Z
dc.date.available2021-02-11T07:53:53Z
dc.date.issued2001
dc.description.abstractPartial duration (peaks over threshold) series have been used as an alternative to annual maxima series in flood frequency analysis. Poisson process is usually assumed for the occurrence of peaks. In some peaks over threshold series, variance of the annual number of exceedances is significantly smaller (or larger) than the mean. In such cases binomial (or negative binomial) distribution has a better fit. Expressions are obtained for the estimation of the T-year flood and its sampling variance when binomial (or negative binomial) model is combined with the exponential distribution of peak magnitudes. It is shown that the results are almost identical to those obtained using the Poisson model, for which much simpler expressions are available.
dc.identifierhttps://www.elibrary.ru/item.asp?id=563698
dc.identifier.citationJournal of Hydrology, 2001, 244, 1-2, 86-96
dc.identifier.issn0022-1694
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/24651
dc.subjectFLOOD
dc.subjectPARTIAL DURATION SERIES
dc.subjectPEAKS OVER THRESHOLD
dc.subjectPOISSON PROCESS
dc.subjectBINOMIAL DISTRIBUTION
dc.subjectNEGATIVE BINOMIAL DISTRIBUTION
dc.titleEFFECT OF THE OCCURRENCE PROCESS OF THE PEAKS OVER THRESHOLD ON THE FLOOD ESTIMATES
dc.typeСтатья

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