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dc.contributor.authorBardsley, W. Earlen_NZ
dc.date.accessioned2016-05-26T02:00:48Z
dc.date.available2016en_NZ
dc.date.available2016-05-26T02:00:48Z
dc.date.issued2016en_NZ
dc.identifier.citationBardsley, W. E. (2016). Cautionary note on multi-component flood distributions for annual maxima. Hydrological Processes. http://doi.org/10.1002/hyp.10886en
dc.identifier.issn0885-6087en_NZ
dc.identifier.urihttps://hdl.handle.net/10289/10263
dc.description.abstractMulti-component probability distributions such as the two-component Gumbel distribution are sometimes applied to annual flood maxima when individual floods are seen as belonging to different classes, depending on physical processes or time of year. However, hydrological inconsistencies may arise if only non-classified annual maxima are available to estimate the component distribution parameters. In particular, an unconstrained best fit to annual flood maxima may yield some component distributions with a high probability of simulating floods with negative discharge. In such situations multi-component distributions cannot be justified as an improved approximation to a local physical reality of mixed flood types, even though a good data fit is achieved. This effect usefully illustrates that a good match to data is no guarantee against degeneracy of hydrological models.en_NZ
dc.format.mimetypeapplication/pdf
dc.language.isoen
dc.publisherWileyen_NZ
dc.relation.urihttp://onlinelibrary.wiley.com/doi/10.1002/hyp.10886/abstract;jsessionid=B49F0A85C0975C444A505DCD10796A78.f02t01en_NZ
dc.rightsThis article has been accepted for publication and undergone full peer review but has not been through the copyediting, typesetting, pagination and proofreading process, which may lead to differences between this version and the Version of Record. Please cite this article as doi: 10.1002/hyp.10886
dc.subjectflood maximaen_NZ
dc.subjectmulti-component distributionen_NZ
dc.subjectparameter erroren_NZ
dc.subjecttwo-component extreme value distributionen_NZ
dc.titleCautionary note on multi-component flood distributions for annual maximaen_NZ
dc.typeJournal Article
dc.identifier.doi10.1002/hyp.10886en_NZ
dc.relation.isPartOfHydrological Processesen_NZ
pubs.elements-id138881


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