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dc.contributor.authorRagulina, Galina
dc.contributor.authorReitan, Trond
dc.date.accessioned2017-06-23T11:05:49Z
dc.date.available2017-06-23T11:05:49Z
dc.date.created2017-01-20T07:33:40Z
dc.date.issued2017
dc.identifier.issn0262-6667
dc.identifier.urihttp://hdl.handle.net/11250/2446795
dc.description.abstractAssessing the probability of extreme precipitation events is consequential in civil planning. This requires an understanding of how return values change with return periods, which is essentially described by the generalized extreme value (GEV) shape parameter. Some works in the field suggest a constant shape parameter, while our analysis indicates a non-universal value. We re-analysed an older precipitation dataset (169 stations) extended by Norwegian data (71 stations). We showed that while each set seems to have a constant shape parameter, it differs between the two datasets, indicating regional differences. For a more comprehensive analysis of spatial effects, we examined a global dataset (1495 stations). We provided shape parameter maps for two models and found clear evidence that the shape parameter depends on elevation, while the effect of latitude remains uncertain. Our results confirm an explanation in terms of dominating precipitation systems based on a proxy derived from the Köppen-Geiger climate classification.
dc.language.isoeng
dc.relation.urihttp://dx.doi.org/10.1080/02626667.2016.1260134
dc.titleGeneralized extreme value shape parameter and its nature for extreme precipitation using long time series and the Bayesian approach
dc.typePeer reviewed
dc.typeJournal article
dc.source.journalHydrological Sciences Journal
dc.identifier.doi10.1080/02626667.2016.1260134
dc.identifier.cristin1432958
cristin.unitcode7452,20,0,0
cristin.unitnameNaturskade
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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