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dc.contributor.authorMushtaq, Sumra
dc.contributor.authorMiniussi, Arianna
dc.contributor.authorMerz, Ralf
dc.contributor.authorTarasova, Larisa
dc.contributor.authorMarra, Francesco
dc.contributor.authorBasso, Stefano
dc.date.accessioned2024-01-25T08:54:06Z
dc.date.available2024-01-25T08:54:06Z
dc.date.created2023-11-13T14:51:14Z
dc.date.issued2023
dc.identifier.citationGeophysical Research Letters. 2023, 50 (20), e2023GL105429.en_US
dc.identifier.issn0094-8276
dc.identifier.urihttps://hdl.handle.net/11250/3113705
dc.description.abstractRiver floods are generated by various processes that, if disregarded, may induce errors in flood hazard assessment. This is particularly relevant where events extraordinarily larger than the typical floods have been observed, that is, for rivers with a flood divide in their flood-frequency curves. We identify 11 such cases in a large set of German catchments and test a statistical approach that accounts for different runoff-generation processes to predict the magnitude and frequency of extraordinarily high floods. We observe that in catchments with a flood divide, ordinary peaks are generated by different runoff-generation processes and the distribution of at least one process is heavy-tailed. By accounting for the different tail behaviors of multiple processes, we can reproduce flood-frequency curves in these catchments. Our findings shed light on the origin of flood divides and set a method to improve the estimation of high flood quantiles in these high-risk cases.en_US
dc.language.isoengen_US
dc.publisherWileyen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titlePrediction of Extraordinarily High Floods Emerging From Heterogeneous Flow Generation Processesen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holder© 2023 The Authorsen_US
dc.source.pagenumber10en_US
dc.source.volume50en_US
dc.source.journalGeophysical Research Lettersen_US
dc.source.issue20en_US
dc.identifier.doi10.1029/2023GL105429
dc.identifier.cristin2195957
dc.source.articlenumbere2023GL105429en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


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