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dc.contributor.authorKing, Martin Peter
dc.contributor.authorLi, Camille
dc.contributor.authorSobolowski, Stefan Pieter
dc.date.accessioned2022-04-26T08:15:38Z
dc.date.available2022-04-26T08:15:38Z
dc.date.created2021-08-16T16:33:40Z
dc.date.issued2021
dc.identifier.urihttps://hdl.handle.net/11250/2992722
dc.description.abstractWe re-examine the uncertainty of the El Niño–Southern Oscillation (ENSO) teleconnection to the North Atlantic following the investigation of Deser et al. (2017) (DES2017). Our analyses are performed on the November–December (ND) and January–February (JF) means separately and for a geographical area that covers a larger extent in the midlatitude North Atlantic than DES2017. The motivation for splitting the cold season in this way arises from the fact that the teleconnection patterns and underlying physical mechanisms are different in late fall compared to midwinter. As in DES2017, our main technique in quantifying the uncertainty is bootstrap resampling. Amplitudes and spatial correlations of the bootstrap samples are presented together effectively using Taylor diagrams. In addition to the confidence intervals calculated from Student's t tests and the percentiles of anomalous sea level pressure (SLP) values in the bootstrap samples, we also investigate additional confidence intervals using techniques that are not widely used in climate research but have different advantages. In contrast to the interpretation by DES2017, our results indicate that we can have confidence (at the 5 % significance level) in the patterns of the teleconnected SLP anomalies. The uncertainties in the amplitudes remain large, with the upper-percentile anomalies at up to 2 times those of the lower percentiles in the North Pacific and 2.8 times in the North Atlantic.en_US
dc.language.isoengen_US
dc.publisherCopernicus Publicationsen_US
dc.relation.urihttps://wcd.copernicus.org/articles/2/759/2021/wcd-2-759-2021.html
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleResampling of ENSO teleconnections: accounting for cold-season evolution reduces uncertainty in the North Atlanticen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright Author(s) 2021en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.doi10.5194/wcd-2-759-2021
dc.identifier.cristin1926434
dc.source.journalWeather and Climate Dynamics (WCD)en_US
dc.source.pagenumber759-776en_US
dc.relation.projectNorges forskningsråd: 255027en_US
dc.relation.projectNorges forskningsråd: 275268en_US
dc.subject.nsiVDP::Meteorologi: 453en_US
dc.subject.nsiVDP::Meteorology: 453en_US
dc.identifier.citationWeather and Climate Dynamics. 2021, 2 (3), 759-776.en_US
dc.source.volume2en_US
dc.source.issue3en_US


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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal