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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSGUBIN, Giovanni
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSWINGEDOUW, Didier
hal.structure.identifierRoyal Netherlands Meteorological Institute [KNMI]
dc.contributor.authorDRIJFHOUT, Sybren
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMARY, Yannick
hal.structure.identifierInstitut de Mécanique et d'Ingénierie [I2M]
dc.contributor.authorBENNABI, Amine
dc.date.accessioned2024-10-07T08:34:43Z
dc.date.available2024-10-07T08:34:43Z
dc.date.issued2017-02-15
dc.identifier.issn2041-1723en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/202272
dc.description.abstractEnObservations over the 20th century evidence no long-term warming in the subpolar North Atlantic (SPG). This region even experienced a rapid cooling around 1970, raising a debate over its potential reoccurrence. Here we assess the risk of future abrupt SPG cooling in 40 climate models from the fifth Coupled Model Intercomparison Project (CMIP5). Contrary to the long-term SPG warming trend evidenced by most of the models, 17.5% of the models (7/40) project a rapid SPG cooling, consistent with a collapse of the local deep-ocean convection. Uncertainty in projections is associated with the models' varying capability in simulating the present-day SPG stratification, whose realistic reproduction appears a necessary condition for the onset of a convection collapse. This event occurs in 45.5% of the 11 models best able to simulate the observed SPG stratification. Thus, due to systematic model biases, the CMIP5 ensemble as a whole underestimates the chance of future abrupt SPG cooling, entailing crucial implications for observation and adaptation policy.
dc.description.sponsorshipLabEx Institut Pierre Simon Laplace (IPSL): Understand climate and anticipate future changes - ANR-10-LABX-0018en_US
dc.language.isoENen_US
dc.rights.urihttp://creativecommons.org/licenses/by/
dc.title.enAbrupt cooling over the North Atlantic in modern climate models
dc.typeArticle de revueen_US
dc.identifier.doi10.1038/ncomms14375en_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Climatologieen_US
dc.description.sponsorshipEuropeEarth system Model Bias Reduction and assessing Abrupt Climate changeen_US
dc.description.sponsorshipEuropeInfrastructure for the European Network for Earth System modelling - Phase 2en_US
dc.description.sponsorshipEuropeBlue-Action: Arctic impact on weather and climaten_US
bordeaux.journalNature Communicationsen_US
bordeaux.page14375en_US
bordeaux.volume8en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifiercea-02138768
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccCC BYen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Nature%20Communications&rft.date=2017-02-15&rft.volume=8&rft.spage=14375&rft.epage=14375&rft.eissn=2041-1723&rft.issn=2041-1723&rft.au=SGUBIN,%20Giovanni&SWINGEDOUW,%20Didier&DRIJFHOUT,%20Sybren&MARY,%20Yannick&BENNABI,%20Amine&rft.genre=article


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