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dc.rights.licenseopenen_US
hal.structure.identifierXi'an Jiaotong University [Xjtu]
dc.contributor.authorBRAHIM, Yassine Ait
hal.structure.identifierMax Planck Institute for Chemistry [MPIC]
dc.contributor.authorWASSENBURG, Jasper
hal.structure.identifierUniversidade de São Paulo = University of São Paulo [USP]
dc.contributor.authorCRUZ, Francisco
hal.structure.identifierVariabilité à long terme du climat de l'océan [VALCO]
dc.contributor.authorSIFEDDINE, Abdel
hal.structure.identifierJohannes Gutenberg - Universität Mainz = Johannes Gutenberg University [JGU]
dc.contributor.authorSCHOLZ, Denis
hal.structure.identifierUniversité Ibn Zohr [Agadir]
dc.contributor.authorBOUCHAOU, Lhoussaine
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorDASSIE, Emilie
hal.structure.identifierMax Planck Institute for Chemistry [MPIC]
dc.contributor.authorJOCHUM, Klaus
hal.structure.identifierMax Planck Institute for Chemistry [MPIC]
dc.contributor.authorEDWARDS, R. Lawrence
hal.structure.identifierXi'an Jiaotong University [Xjtu]
hal.structure.identifierUniversity of Minnesota [Twin Cities] [UMN]
dc.contributor.authorCHENG, Hai
dc.date.accessioned2024-03-13T09:44:19Z
dc.date.available2024-03-13T09:44:19Z
dc.date.issued2018
dc.identifier.issn2045-2322en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/188761
dc.description.abstractEnHere we present a new composite record from two well-dated speleothem records from two caves in Northern Morocco. The high-resolution record covers the last millennium allowing to detect multi-decadal to centennial periodicities. Over the industrial period, δ18O values of our speleothems are shown to be dominated by the main mode of decadal variability in the North Atlantic region: the North Atlantic Oscillation (NAO). Statistical analyses confirm the previously reported multi-decadal variability related to the influence of the Atlantic Multidecadal Oscillation (AMO) in the region. High power and persistent centennial-scale periodicities, similar to the Vries-Suess 200-year solar cycle, are observed as well. Indeed, comparison between solar activity reconstructions and our record confirms the in-phase relationship on centennial time-scales. Low δ18O values, and hence negative phases of NAO that bring precipitation towards the Western Mediterranean, are observed during well-known solar minima periods. The results are consistent with previous models which describe low irradiance as a trigger for southward shifts of precipitation-bearing westerlies during winter.
dc.language.isoENen_US
dc.subject.enPalaeoclimate
dc.title.enMulti-decadal to centennial hydro-climate variability and linkage to solar forcing in the Western Mediterranean during the last 1000 years
dc.typeArticle de revueen_US
dc.identifier.doi10.1038/s41598-018-35498-xen_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Climatologieen_US
bordeaux.journalScientific Reportsen_US
bordeaux.page17446en_US
bordeaux.volume8en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue1en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-01950053
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=Scientific%20Reports&rft.date=2018&rft.volume=8&rft.issue=1&rft.spage=17446&rft.epage=17446&rft.eissn=2045-2322&rft.issn=2045-2322&rft.au=BRAHIM,%20Yassine%20Ait&WASSENBURG,%20Jasper&CRUZ,%20Francisco&SIFEDDINE,%20Abdel&SCHOLZ,%20Denis&rft.genre=article


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