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Monsoonal Forcing of European Ice‐Sheet Dynamics During the Late Quaternary

dc.rights.licenseopenen_US
dc.contributor.authorKABOTH‐BAHR, Stefanie
hal.structure.identifierUniversität Heidelberg [Heidelberg] = Heidelberg University
dc.contributor.authorBAHR, Andre
hal.structure.identifierInstitut de Mécanique Céleste et de Calcul des Ephémérides [IMCCE]
dc.contributor.authorZEEDEN, Christian
hal.structure.identifierUnité Géosciences Marines [GM]
dc.contributor.authorTOUCANNE, Samuel
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorEYNAUD, Frederique
dc.contributor.authorJIMÉNEZ‐ESPEJO, Francisco
dc.contributor.authorRÖHL, Ursula
hal.structure.identifierNational Oceanography Centre [Southampton] [NOC]
dc.contributor.authorFRIEDRICH, Oliver
hal.structure.identifierFederal Institute of Hydrology (BfG)
dc.contributor.authorPROSS, Jörg
dc.contributor.authorLÖWEMARK, Ludvig
hal.structure.identifierUniversiteit Utrecht / Utrecht University [Utrecht]
dc.contributor.authorLOURENS, Lucas
dc.date.accessioned2024-05-03T14:34:09Z
dc.date.available2024-05-03T14:34:09Z
dc.date.issued2018-07-24
dc.identifier.issn0094-8276en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/199614
dc.description.abstractEnThe dynamics of Northern Hemisphere ice sheets during Late Quaternary glacials have yet been dominantly examined from a Laurentide Ice Sheet perspective, which helped shaping the idea of moisture-starved glacials and small-scale ice volume variability. However, the waxing and waning of the European Ice Sheet (EIS) casts doubt on this perception. Understanding EIS dynamics under glacial boundary conditions is crucial because its meltwater pulses influence global climate by weakening deepwater formation in the North Atlantic Ocean. Here we show that the advection of subtropical water toward the continental margin of western Europe lead to enhanced moisture availability on the continent and fueled the growth of EIS lobes during glacials. This warm-water pooling was caused by monsoonally paced enhanced Mediterranean Outflow Water (MOW) entrainment that dragged subtropical surface waters toward the European margin. This mechanism presents a yet unrecognized marine-terrestrial pathway that allows low-latitude forcing to shape high-latitude glaciations.
dc.language.isoENen_US
dc.rights.urihttp://hal.archives-ouvertes.fr/licences/copyright/
dc.title.enMonsoonal Forcing of European Ice‐Sheet Dynamics During the Late Quaternary
dc.typeArticle de revueen_US
dc.identifier.doi10.1029/2018GL078751en_US
dc.subject.halPhysique [physics]en_US
dc.subject.halPlanète et Univers [physics]/Astrophysique [astro-ph]en_US
bordeaux.journalGeophysical Research Lettersen_US
bordeaux.page7066-7074en_US
bordeaux.volume45en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue14en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-02308052
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=2018-07-24&rft.volume=45&rft.issue=14&rft.spage=7066-7074&rft.epage=7066-7074&rft.eissn=0094-8276&rft.issn=0094-8276&rft.au=KABOTH%E2%80%90BAHR,%20Stefanie&BAHR,%20Andre&ZEEDEN,%20Christian&TOUCANNE,%20Samuel&EYNAUD,%20Frederique&rft.genre=article


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