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dc.contributor.authorPolyakov, Igor V.eng
dc.contributor.authorBeszczynska-Möller, Agnieszkaeng
dc.contributor.authorCarmack, Eddy C.eng
dc.contributor.authorDmitreko, Igor A.eng
dc.contributor.authorFahrbach, E.eng
dc.contributor.authorFrolov, Ivan E.eng
dc.contributor.authorGerdes, Rüdigereng
dc.contributor.authorHansen, Edmondeng
dc.contributor.authorHolfort, Jürgeneng
dc.contributor.authorIvanov, Vladimir V.eng
dc.contributor.authorJohnson, Mark A.eng
dc.contributor.authorKarcher, Michaeleng
dc.contributor.authorKauker, Frankeng
dc.contributor.authorMorison, Jameseng
dc.contributor.authorOrvik, Kjell Arildeng
dc.contributor.authorSchauer, Ursulaeng
dc.contributor.authorSimmons, Harper L.eng
dc.contributor.authorSkagseth, Øysteineng
dc.contributor.authorSokolov, Vladimir T.eng
dc.contributor.authorSteele, Michaeleng
dc.contributor.authorTimokhov, Leonid A.eng
dc.contributor.authorWalsh, Davideng
dc.contributor.authorWalsh, John E.eng
dc.date.accessioned2005-09-12T11:41:59Z
dc.date.available2005-09-12T11:41:59Z
dc.date.issued2005-09-09eng
dc.PublishedGeophysical Research Letters 2005 32 L17605en
dc.identifier.issn0094-8276en_US
dc.identifier.urihttps://hdl.handle.net/1956/786
dc.description.abstractThis study was motivated by a strong warming signal seen in mooring-based and oceanographic survey data collected in 2004 in the Eurasian Basin of the Arctic Ocean. The source of this and earlier Arctic Ocean changes lies in interactions between polar and sub-polar basins. Evidence suggests such changes are abrupt, or pulse-like, taking the form of propagating anomalies that can be traced to higher-latitudes. For example, an anomaly found in 2004 in the eastern Eurasian Basin took ~1.5 years to propagate from the Norwegian Sea to the Fram Strait region, and additional ~4.5–5 years to reach the Laptev Sea slope. While the causes of the observed changes will require further investigation, our conclusions are consistent with prevailing ideas suggesting the Arctic Ocean is in transition towards a new, warmer state.en_US
dc.format.extent194371 byteseng
dc.format.mimetypeapplication/pdfeng
dc.language.isoengeng
dc.publisherAmerican Geophysical Unionen_US
dc.titleOne more step toward a warmer Arcticen_US
dc.typePeer reviewed
dc.typeJournal article
dc.identifier.doihttps://doi.org/10.1029/2005gl023740


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