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dc.contributor.authorBreivik, Øyvindeng
dc.contributor.authorAarnes, Ole Johaneng
dc.contributor.authorAbdalla, Saleheng
dc.contributor.authorBidlot, Jean-Raymondeng
dc.contributor.authorJanssen, Peter A. E. M.eng
dc.date.accessioned2015-01-26T12:12:31Z
dc.date.available2015-01-26T12:12:31Z
dc.date.issued2014-07eng
dc.identifier.issn1944-8007en_US
dc.identifier.urihttps://hdl.handle.net/1956/9254
dc.description.abstractGlobal return values of marine wind speed and significant wave height are estimated from very large aggregates of archived ensemble forecasts at +240 h lead time. Long lead time ensures that the forecasts represent independent draws from the model climate. Compared with ERA-Interim, a reanalysis, the ensemble yields higher return estimates for both wind speed and significant wave height. Confidence intervals are much tighter due to the large size of the data set. The period (9 years) is short enough to be considered stationary even with climate change. Furthermore, the ensemble is large enough for nonparametric 100 year return estimates to be made from order statistics. These direct return estimates compare well with extreme value estimates outside areas with tropical cyclones. Like any method employing modeled fields, it is sensitive to tail biases in the numerical model, but we find that the biases are moderate outside areas with tropical cyclones.en_US
dc.language.isoengeng
dc.publisherWileyen_US
dc.publisherAmerican Geophysical Unionen_US
dc.subjectreturn valueseng
dc.subjectextreme value analysiseng
dc.subjectmarine windeng
dc.subjectsignificant wave heighteng
dc.subjectensemble predictioneng
dc.titleWind and wave extremes over the world oceans from very large ensemblesen_US
dc.typePeer reviewed
dc.typeJournal article
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2014 American Geophysical Union. All Rights Reserved.en_US
dc.identifier.doihttps://doi.org/10.1002/2014gl060997
dc.source.journalGeophysical Research Letters
dc.source.4041
dc.source.1414
dc.source.pagenumber5122-5131


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