NON-STATIONARY APPROACH TO AT-SITE FLOOD FREQUENCY MODELLING II. WEIGHTED LEAST SQUARES ESTIMATION

dc.contributor.authorStrupczewski W.G.
dc.contributor.authorKaczmarek Z.
dc.date.accessioned2021-03-10T04:26:10Z
dc.date.available2021-03-10T04:26:10Z
dc.date.issued2001
dc.description.abstractThis is the second of the three-part paper and generalises the least squares method to the weighted least squares (WLS) method in order to deal with the trend in the first two moments. The generalised method applies when the assumption of constant variance does not hold and the functional form of a trend in the variance is given. In the generalised method, the parameters of trend in the mean and variance are estimated simultaneously. To keep the weights as power functions of variances only, the restrictions on distribution functions are formulated, which, in fact, are not difficult to fulfil in hydrological studies. It is shown that the WLS method coincides with the maximum likelihood method in the case of the normal distribution.
dc.identifierhttps://www.elibrary.ru/item.asp?id=689462
dc.identifier.citationJournal of Hydrology, 2001, 248, 1-4, 143-151
dc.identifier.issn0022-1694
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/26521
dc.subjectTIME SERIES
dc.subjectTREND
dc.subjectLEAST SQUARES METHOD
dc.subjectRIVER
dc.subjectFLOODS
dc.subjectFREQUENCY
dc.titleNON-STATIONARY APPROACH TO AT-SITE FLOOD FREQUENCY MODELLING II. WEIGHTED LEAST SQUARES ESTIMATION
dc.typeСтатья

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