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dc.contributor.authorNilsen, Tine
dc.contributor.authorRypdal, Kristoffer
dc.contributor.authorFredriksen, Hege-Beate
dc.date.accessioned2017-02-24T15:08:56Z
dc.date.available2017-02-24T15:08:56Z
dc.date.issued2016-04-28
dc.description.abstractIn this article it is discussed how temperature variability on centennial timescales and longer can be described in a simplistic way. By analysing the scaling in late Holocene temperature reconstructions and longer temperature records from Greenland and Antarctic ice cores, we find that the choice of model depends heavily on the data material and timescale one chooses to emphasize. Ignoring data beyond the Holocene seems plausible when predicting temperature, but not for other purposes.en_US
dc.descriptionPublished version. Source at <a href=http://dx.doi.org/10.5194/esd-7-419-2016> http://dx.doi.org/10.5194/esd-7-419-2016 </a>en_US
dc.identifier.citationNilsen T, Rypdal K, Fredriksen H. Are there multiple scaling regimes in Holocene temperature records?. Earth System Dynamics. 2016;7(2):419-439en_US
dc.identifier.issn2190-4979
dc.identifier.issn2190-4987
dc.identifier.otherFRIDAID 1353745
dc.identifier.other10.5194/esd-7-419-2016
dc.identifier.urihttps://hdl.handle.net/10037/10364
dc.language.isoengen_US
dc.publisherEuropean Geosciences Unionen_US
dc.relation.journalEarth System Dynamics
dc.relation.projectIDinfo:eu-repo/grantAgreement/RCN/KLIMAFORSK/229754/Norway/Long-range memory in Earths climate response and its implications for future global warming//en_US
dc.relation.urihttp://www.earth-syst-dynam.net/7/419/2016/esd-7-419-2016.html
dc.rights.accessRightsopenAccessen_US
dc.subjectVDP::Matematikk og naturvitenskap: 400::Matematikk: 410::Anvendt matematikk: 413en_US
dc.subjectPaleoklima / Paleoclimateen_US
dc.titleAre there multiple scaling regimes in Holocene temperature records?en_US
dc.typeJournal articleen_US
dc.typeTidsskriftartikkelen_US
dc.typePeer revieweden_US


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