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dc.rights.licenseopenen_US
hal.structure.identifierUniversity of Tromsø [UiT]
dc.contributor.authorFAUST, Johan
hal.structure.identifierThe Arctic University of Norway [Tromsø, Norway] [UiT]
dc.contributor.authorFABIAN, Karl
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMILZER, Gesa
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorGIRAUDEAU, Jacques
hal.structure.identifierThe Arctic University of Norway [Tromsø, Norway] [UiT]
dc.contributor.authorKNIES, Jochen
dc.date.accessioned2024-10-11T09:44:15Z
dc.date.available2024-10-11T09:44:15Z
dc.date.issued2016
dc.identifier.issn0012-821Xen_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/202430
dc.description.abstractEnThe North Atlantic Oscillation (NAO) is the leading mode of atmospheric circulation variability in the North Atlantic region. Associated shifts of storm tracks, precipitation and temperature patterns affect energy supply and demand, fisheries and agricultural, as well as marine and terrestrial ecological dynamics. Long-term NAO records are crucial to better understand its response to climate forcing factors, and assess predictability and shifts associated with ongoing climate change. A recent study of instrumental time series revealed NAO as main factor for a strong relation between winter temperature, precipitation and river discharge in central Norway over the past 50 years. Here we compare geochemical measurements with instrumental data and show that primary productivity recorded in central Norwegian fjord sediments is sensitive to NAO variability. This observation is used to calibrate paleoproductivity changes to a 500-year reconstruction of winter NAO (Luterbacher et al., 2001). Conditioned on a stationary relation between our climate proxy and the NAO we establish a first high resolution NAO proxy record (NAO TFJ) from marine sediments covering the past 2800 years. The NAO TFJ shows distinct co-variability with climate changes over Greenland, solar activity and Northern Hemisphere glacier dynamics as well as climatically associated paleo-demographic trends. The here presented climate record shows that fjord sediments provide crucial information for an improved understanding of the linkages between atmospheric circulation, solar and oceanic forcing factors.
dc.language.isoENen_US
dc.subject.enMarine Sediments
dc.subject.enNAO
dc.subject.enTrondheimsfjord
dc.subject.enNorway
dc.title.enNorwegian fjord sediments reveal NAO related winter temperature and precipitation changes of the past 2800 years
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.epsl.2015.12.003en_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Climatologieen_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Océanographieen_US
dc.subject.halPlanète et Univers [physics]/Océan, Atmosphèreen_US
bordeaux.journalEarth and Planetary Science Lettersen_US
bordeaux.page84-93en_US
bordeaux.volume435en_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-02128902
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=Earth%20and%20Planetary%20Science%20Letters&rft.date=2016&rft.volume=435&rft.spage=84-93&rft.epage=84-93&rft.eissn=0012-821X&rft.issn=0012-821X&rft.au=FAUST,%20Johan&FABIAN,%20Karl&MILZER,%20Gesa&GIRAUDEAU,%20Jacques&KNIES,%20Jochen&rft.genre=article


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