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dc.rights.licenseopenen_US
dc.contributor.authorMÉNÉGOZ, Martin
dc.contributor.authorCASSOU, Christophe
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSWINGEDOUW, Didier
dc.contributor.authorRUPRICH-ROBERT, Yohan
dc.contributor.authorBRETONNIÈRE, Pierre-Antoine
dc.contributor.authorDOBLAS-REYES, Francisco
dc.date.accessioned2024-05-06T09:12:24Z
dc.date.available2024-05-06T09:12:24Z
dc.date.issued2017-11-09
dc.identifier.issn0930-7575en_US
dc.identifier.urihttps://pub.orcid.org/v2.1/0000-0002-4008-2026/work/38861390
dc.identifier.urioai:crossref.org:10.1007/s00382-017-3986-1
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/199638
dc.description.abstractEnThe modulation by the Atlantic multidecadal variability (AMV) of the dynamical climate response to a Pinatubo-like eruption is investigated for the boreal winter season based on a suite of large ensemble experiments using the CNRM-CM5 Coupled Global Circulation Model. The volcanic eruption induces a strong reduction and retraction of the Hadley cell during 2 years following the eruption and independently of the phase of the AMV. The mean extratropical westerly circulation simultaneously weakens throughout the entire atmospheric column, except at polar Northern latitudes where the zonal circulation is slightly strengthened. Yet, there are no significant changes in the modes of variability of the surface atmospheric circulation, such as the North Atlantic Oscillation (NAO), in the first and the second winters after the eruption. Significant modifications over the North Atlantic sector are only found during the third winter. Using clustering techniques, we decompose the atmospheric circulation into weather regimes and provide evidence for inhibition of the occurrence of negative NAO-type circulation in response to volcanic forcing. This forced signal is amplified in cold AMV conditions and is related to sea ice/atmosphere feedbacks in the Arctic and to tropical-extratropical teleconnections. Finally, we demonstrate that large ensembles of simulations are required to make volcanic fingerprints emerge from climate noise at mid-latitudes. Using small size ensemble could easily lead to misleading conclusions especially those related to the extratropical dynamics, and specifically the NAO.
dc.language.isoENen_US
dc.sourceorcid
dc.sourcecrossref
dc.subject.enVolcanic eruptions
dc.subject.enClimate dynamics
dc.subject.enNorth Atlantic
dc.subject.enOscillation
dc.subject.enAtlantic multidecadal variability
dc.subject.enEnsemble size
dc.subject.enClimate model
dc.title.enRole of the Atlantic Multidecadal Variability in modulating the climate response to a Pinatubo-like volcanic eruption
dc.typeArticle de revueen_US
dc.identifier.doi10.1007/s00382-017-3986-1en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalClimate Dynamicsen_US
bordeaux.page1863-1883en_US
bordeaux.volume51en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue5-6en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.identifierhal-04569149
hal.version1
hal.date.transferred2024-05-06T09:12:26Z
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exporttrue
workflow.import.sourcedissemin
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Climate%20Dynamics&rft.date=2017-11-09&rft.volume=51&rft.issue=5-6&rft.spage=1863-1883&rft.epage=1863-1883&rft.eissn=0930-7575&rft.issn=0930-7575&rft.au=M%C3%89N%C3%89GOZ,%20Martin&CASSOU,%20Christophe&SWINGEDOUW,%20Didier&RUPRICH-ROBERT,%20Yohan&BRETONNI%C3%88RE,%20Pierre-Antoine&rft.genre=article


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