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dc.contributor.authorRisebrobakken, Bjørgeng
dc.contributor.authorJansen, Eysteineng
dc.contributor.authorAndersson, Carineng
dc.contributor.authorMjelde, Eirikeng
dc.contributor.authorHevrøy, Kjerstieng
dc.date.accessioned2004-08-11T08:10:33Z
dc.date.accessioned2004-08-26T11:57:21Z
dc.date.available2004-08-11T08:10:33Zen
dc.date.available2004-08-26T11:57:21Z
dc.date.issued2003-03-26eng
dc.PublishedPaleoceanography 2003 18(1): 1017en
dc.identifier.issn0883-8305en_US
dc.identifier.urihttps://hdl.handle.net/1956/364
dc.description.abstractHigh-resolution records from IMAGES core MD95-2011 in the eastern Norwegian Sea provide evidence for relatively large- and small-scale high-latitude climate variability throughout the Holocene. During the early and mid-Holocene a situation possibly driven by consistent stronger westerlies increased the eastward influence of Arctic intermediate and near-surface waters. For the late Holocene a relaxation of the atmospheric forcing resulted in increased influence of Atlantic water. The main changes in Holocene climate show no obvious connection to changing solar irradiance, and spectral analysis reveals no consistent signature for any periodic behavior of Holocene climate at millennial or centennial timescales. There are, however, indications of consistent multidecadal variability.en_US
dc.format.extent55749 byteseng
dc.format.extent137 byteseng
dc.format.extent2452278 byteseng
dc.format.mimetypetext/plaineng
dc.format.mimetypetext/plaineng
dc.format.mimetypeapplication/pdfeng
dc.language.isoengeng
dc.publisherAmerican Geophysical Unionen_US
dc.titleA high-resolution study of Holocene paleoclimatic and paleoceanographic changes in the Nordic Seasen_US
dc.typePeer reviewed
dc.typeJournal article
dc.rights.holderCopyright 2003 the American Geophysical Unionen_US
dc.identifier.doihttps://doi.org/10.1029/2002pa000764


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