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Regional seesaw between the North Atlantic and Nordic Seas during the last glacial abrupt climate events

dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorWARY, Melanie
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorEYNAUD, Frederique
IDREF: 144113570
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSWINGEDOUW, Didier
dc.contributor.authorMASSON-DELMOTTE, Valérie
dc.contributor.authorMATTHIESSEN, Jens
dc.contributor.authorKISSEL, Catherine
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorZUMAQUE, Jena
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorROSSIGNOL, Linda
dc.contributor.authorJOUZEL, Jean
dc.date.accessioned2024-05-29T08:07:08Z
dc.date.available2024-05-29T08:07:08Z
dc.date.issued2017-06-30
dc.identifier.issn1814-9324en_US
dc.identifier.urioai:crossref.org:10.5194/cp-13-729-2017
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/200115
dc.description.abstractEnAbstract. Dansgaard–Oeschger oscillations constitute one of the most enigmatic features of the last glacial cycle. Their cold atmospheric phases have been commonly associated with cold sea-surface temperatures and expansion of sea ice in the North Atlantic and adjacent seas. Here, based on dinocyst analyses from the 48–30 ka interval of four sediment cores from the northern Northeast Atlantic and southern Norwegian Sea, we provide direct and quantitative evidence of a regional paradoxical seesaw pattern: cold Greenland and North Atlantic phases coincide with warmer sea-surface conditions and shorter seasonal sea-ice cover durations in the Norwegian Sea as compared to warm phases. Combined with additional palaeorecords and multi-model hosing simulations, our results suggest that during cold Greenland phases, reduced Atlantic meridional overturning circulation and cold North Atlantic sea-surface conditions were accompanied by the subsurface propagation of warm Atlantic waters that re-emerged in the Nordic Seas and provided moisture towards Greenland summit.
dc.description.sponsorshipGroenland vert - ANR-10-CEPL-0008en_US
dc.language.isoENen_US
dc.rightsAttribution 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/us/*
dc.sourcecrossref
dc.title.enRegional seesaw between the North Atlantic and Nordic Seas during the last glacial abrupt climate events
dc.typeArticle de revueen_US
dc.identifier.doi10.5194/cp-13-729-2017en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalClimate of the Pasten_US
bordeaux.page729-739en_US
bordeaux.volume13en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue6en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcedissemin
dc.rights.ccCC BYen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Climate%20of%20the%20Past&rft.date=2017-06-30&rft.volume=13&rft.issue=6&rft.spage=729-739&rft.epage=729-739&rft.eissn=1814-9324&rft.issn=1814-9324&rft.au=WARY,%20Melanie&EYNAUD,%20Frederique&SWINGEDOUW,%20Didier&MASSON-DELMOTTE,%20Val%C3%A9rie&MATTHIESSEN,%20Jens&rft.genre=article


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