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dc.contributor.authorKeenlyside, Noeleng
dc.contributor.authorOmrani, Nour-Eddineeng
dc.date.accessioned2015-10-06T07:43:24Z
dc.date.available2015-10-06T07:43:24Z
dc.date.issued2014-06-02
dc.PublishedEnvironmental Research Letters 2014, 9(6):061001eng
dc.identifier.issn1748-9326en_US
dc.identifier.urihttps://hdl.handle.net/1956/10545
dc.description.abstractThe rise of global surface temperature waned during the last decade, despite increasing greenhouse gas concentrations. The temperature changes were most pronounced over northern hemisphere land masses during winter (Cohen et al 2012). They were largely associated with weakening of the mid-latitude westerly flow. To some, these temperature changes may seem paradoxical in the light of anthropogenic global warming, and thus there is much interest in explaining them. Peings and Magnusdottir (2014 Environ. Res. Lett. 9 034018) provide evidence that recent warming of the North Atlantic sea surface temperature (SST) may be part of the explanation.en_US
dc.language.isoengeng
dc.publisherIOP Publishingen_US
dc.rightsAttribution CC BYeng
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/eng
dc.subjectAMVeng
dc.subjectClimate changeeng
dc.subjectwinter climateeng
dc.titleHas a warm North Atlantic contributed to recent European cold winters?en_US
dc.typePeer reviewed
dc.typeJournal article
dc.date.updated2015-07-28T11:27:00Z
dc.description.versionpublishedVersionen_US
dc.identifier.doihttps://doi.org/10.1088/1748-9326/9/6/061001
dc.identifier.cristin1154252
dc.subject.nsiVDP::Matematikk og naturvitenskap: 400::Geofag: 450::Meteorologi: 453
dc.subject.nsiVDP::Mathematics and natural scienses: 400::Geosciences: 450::Meteorology: 453
dc.subject.nsiVDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452
dc.subject.nsiVDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452


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