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dc.rights.licenseopenen_US
dc.contributor.authorLINSLEY, Braddock K.
dc.contributor.authorWU, Henry C.
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorDASSIE, Emilie
dc.contributor.authorSCHRAG, Daniel P.
dc.date.accessioned2024-09-16T12:10:18Z
dc.date.available2024-09-16T12:10:18Z
dc.date.issued2015-03-01
dc.identifier.issn0094-8276en_US
dc.identifier.urihttps://www.researchgate.net/publication/273389813_Decadal_Changes_in_South_Pacific_Sea_Surface_Temperatures_and_the_Relationship_to_the_Pacific_Decadal_Oscillation_and_Upper_Ocean_Heat_Content_Decadal_Changes_in_South_Pacific_SST
dc.identifier.urioai:crossref.org:10.1002/2015gl063045
dc.identifier.urioai:researchgate.net:273389813
dc.identifier.uriorcid:0000-0001-8975-5917:10.1002/2015gl063045
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/201602
dc.description.abstractEnDecadal changes in Pacific sea surface temperatures (SST) and upper ocean heat content (OHC) remain poorly understood. We present an annual average composite coral Sr/Ca-derived SST time-series extending back to 1791 from Fiji, Tonga and Rarotonga (FTR) in the Pacific Decadal Oscillation (PDO) sensitive region of the Southwest Pacific. Decadal SST maxima between 1805 and 1830 C.E. indicate unexplained elevated SSTs near the end of the Little Ice Age. The mean period of decadal SST variability in this region has a period near 25 years. Decades of warmer (cooler) FTR SST co-occur with PDO negative (positive) phases since at least ~1930 C.E. and positively correlate with South Pacific OHC (0-700m). FTR SST is also inversely correlated with decadal changes in equatorial Pacific SST as measured by coral Sr/Ca. Collectively, these results support the fluctuating trade wind-shallow meridional overturning cell mechanism for decadal modulation of Pacific SSTs and OHC.
dc.language.isoENen_US
dc.sourcecrossref
dc.sourceresearchgate
dc.sourceorcid
dc.title.enDecadal Changes in South Pacific Sea Surface Temperatures and the Relationship to the Pacific Decadal Oscillation and Upper Ocean Heat Content: Decadal Changes in South Pacific SST
dc.typeArticle de revueen_US
dc.identifier.doi10.1002/2015gl063045en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalGeophysical Research Lettersen_US
bordeaux.page2358-2366en_US
bordeaux.volume42en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue7en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamEAen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.identifierhal-04698834
hal.version1
hal.date.transferred2024-09-16T12:36:05Z
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=Geophysical%20Research%20Letters&rft.date=2015-03-01&rft.volume=42&rft.issue=7&rft.spage=2358-2366&rft.epage=2358-2366&rft.eissn=0094-8276&rft.issn=0094-8276&rft.au=LINSLEY,%20Braddock%20K.&WU,%20Henry%20C.&DASSIE,%20Emilie&SCHRAG,%20Daniel%20P.&rft.genre=article


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