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dc.rights.licenseopenen_US
hal.structure.identifierLaboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] [LSCE]
dc.contributor.authorMARIOTTI, Véronique
hal.structure.identifierLaboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] [LSCE]
hal.structure.identifierModélisation du climat [CLIM]
dc.contributor.authorPAILLARD, Didier
hal.structure.identifierLaboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] [LSCE]
dc.contributor.authorBOPP, Laurent
hal.structure.identifierLaboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] [LSCE]
hal.structure.identifierModélisation du climat [CLIM]
dc.contributor.authorROCHE, Didier M.
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorBOUTTES, Nathaelle
dc.date.accessioned2024-09-19T11:48:57Z
dc.date.available2024-09-19T11:48:57Z
dc.date.issued2016-02-16
dc.identifier.issn0094-8276en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/201686
dc.description.abstractEnChanges in the ventilation of the Southern Ocean are thought to play an important role on deglacial carbon and radiocarbon evolution but have not been tested within a coupled climate-carbon model. Here we present such a simulation based on a simple scenario of transient deglacial sinking of brines-sea ice salt rejections-around Antarctica, which modulates Southern Ocean ventilation. This experiment is able to reproduce deglacial atmospheric changes in carbon and radiocarbon and also ocean radiocarbon records measured in the Atlantic, Southern, and Pacific Oceans. Simulated for the first time in a fully coupled climate-carbon model of intermediate complexity including radiocarbon, our modeling results suggest that the deglacial changes in atmospheric carbon dioxide and radiocarbon were achieved by means of a breakdown in the glacial brine-induced stratification of the Southern Ocean.
dc.language.isoENen_US
dc.title.enA coupled model for carbon and radiocarbon evolution during the last deglaciation
dc.typeArticle de revueen_US
dc.identifier.doi10.1002/2015GL067489en_US
dc.subject.halPlanète et Univers [physics]/Océan, Atmosphèreen_US
dc.subject.halPlanète et Univers [physics]/Interfaces continentales, environnementen_US
bordeaux.journalGeophysical Research Lettersen_US
bordeaux.page1306-1313en_US
bordeaux.volume43en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue3en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-01587469
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Geophysical%20Research%20Letters&rft.date=2016-02-16&rft.volume=43&rft.issue=3&rft.spage=1306-1313&rft.epage=1306-1313&rft.eissn=0094-8276&rft.issn=0094-8276&rft.au=MARIOTTI,%20V%C3%A9ronique&PAILLARD,%20Didier&BOPP,%20Laurent&ROCHE,%20Didier%20M.&BOUTTES,%20Nathaelle&rft.genre=article


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