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dc.contributor.authorBethke, Ingoeng
dc.contributor.authorFurevik, Toreeng
dc.contributor.authorDrange, Helgeeng
dc.date.accessioned2007-02-08T16:22:24Z
dc.date.available2007-02-08T16:22:24Z
dc.date.issued2006-11-14eng
dc.PublishedGeophysical Research Letters 33(21): L21712
dc.identifier.issn0094-8276en_US
dc.identifier.urihttps://hdl.handle.net/1956/2089
dc.description.abstractMost atmosphere-ocean general circulation models (GCMs) forced with increasing greenhouse gas concentrations predict enhanced atmospheric moisture transports to the high northern latitudes. Together with melting of Arctic sea ice and glaciers, this has led to the expectation of a gradual freshening of the northern North Atlantic, tending to reduce the strength of the Atlantic Meridional Overturning Circulation (AMOC). Here a multi-member greenhouse gas GCM experiment is used to demonstrate that both the salinity in the North Atlantic and the inflow of Atlantic Water to the Nordic Seas may increase despite a strong freshening of the Arctic Ocean and a reduced AMOC.en_US
dc.format.extent816760 byteseng
dc.format.mimetypeapplication/pdfeng
dc.language.isoengeng
dc.publisherAmerican Geophysical Unionen_US
dc.titleTowards a more saline North Atlantic and a fresher Arctic under global warmingen_US
dc.typePeer reviewed
dc.typeJournal article
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2006 by the American Geophysical Unionen_US
dc.identifier.doihttps://doi.org/10.1029/2006gl027264
dc.source.journalGeophysical Research Letters
dc.source.4033
dc.source.1421
dc.subject.nsiVDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Oseanografi: 452nob


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