Afficher la notice abrégée

dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
hal.structure.identifierLaboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] [LSCE]
dc.contributor.authorGĂINUŞĂ-BOGDAN, Alina
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSWINGEDOUW, Didier
hal.structure.identifierLaboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] [LSCE]
hal.structure.identifierExtrèmes : Statistiques, Impacts et Régionalisation [ESTIMR]
dc.contributor.authorYIOU, Pascal
hal.structure.identifierCentre national de recherches météorologiques [CNRM]
dc.contributor.authorCATTIAUX, Julien
hal.structure.identifierOcéan et variabilité du climat [VARCLIM]
dc.contributor.authorCODRON, Francis
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMICHEL, Simon
dc.date.accessioned2024-01-23T12:48:36Z
dc.date.available2024-01-23T12:48:36Z
dc.date.issued2020-01
dc.identifier.issn0921-8181en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/187421
dc.description.abstractEnThe mid-Holocene (6,000 years before present) was a warmer period than today in summer in most of the Northern Hemisphere. In winter, over Europe, pollen-based reconstructions show a dipole of temperature anomalies as compared to present-day, with warmer conditions in the north and colder in the south. It has been proposed that this pattern of temperature anomaly could be explained by a persisting positive phase of the North Atlantic Oscillation during this period, which was, however, not reproduced in general by climate models. Indeed, PMIP3 models show a large spread in their response to the mid-Holocene insolation changes, the physical origins of which are not understood. To improve the understanding of the
dc.description.sponsorshipLabEx Institut Pierre Simon Laplace (IPSL): Understand climate and anticipate future changes - ANR-10-LABX-0018en_US
dc.language.isoENen_US
dc.subject.enPMIP3
dc.subject.enAMOC
dc.subject.enNAO
dc.subject.enMid-Holocene
dc.subject.enInter-model spread
dc.title.enAMOC and summer sea ice as key drivers of the spread in mid-holocene winter temperature patterns over Europe in PMIP3 models
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.gloplacha.2019.103055en_US
dc.subject.halPlanète et Univers [physics]/Océan, Atmosphèreen_US
dc.description.sponsorshipEuropeInfrastructure for the European Network for Earth System modelling - Phase 2en_US
bordeaux.journalGlobal and Planetary Changeen_US
bordeaux.page103055en_US
bordeaux.volume184en_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.identifierhal-02346168
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=Global%20and%20Planetary%20Change&rft.date=2020-01&rft.volume=184&rft.spage=103055&rft.epage=103055&rft.eissn=0921-8181&rft.issn=0921-8181&rft.au=G%C4%82INU%C5%9E%C4%82-BOGDAN,%20Alina&SWINGEDOUW,%20Didier&YIOU,%20Pascal&CATTIAUX,%20Julien&CODRON,%20Francis&rft.genre=article


Fichier(s) constituant ce document

Thumbnail

Ce document figure dans la(les) collection(s) suivante(s)

Afficher la notice abrégée