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dc.rights.licenseopenen_US
dc.contributor.authorD’OLIVO, Juan P.
dc.contributor.authorZINKE, Jens
dc.contributor.authorGOYAL, Rishav
dc.contributor.authorENGLAND, Matthew H.
dc.contributor.authorPURICH, Ariaan
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCORREGE, Thierry
dc.contributor.authorZORITA, Eduardo
dc.contributor.authorSCHOLZ, Denis
dc.contributor.authorWEBER, Michael
dc.contributor.authorCARRIQUIRY, José D.
dc.date.accessioned2024-10-23T07:21:56Z
dc.date.available2024-10-23T07:21:56Z
dc.date.issued2024-08-14
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/202688
dc.description.abstractEnThe southwestern tropical Pacific is a key center for the Interdecadal Pacific Oscillation (IPO), which regulates global climate. This study introduces a groundbreaking 627-year coral Sr/Ca sea surface temperature reconstruction from Fiji, representing the IPO’s southwestern pole. Merging this record with other Fiji and central tropical Pacific records, we reconstruct the SST gradient between the southwestern and central Pacific (SWCP), providing a reliable proxy for IPO variability from 1370 to 1997. This reconstruction reveals distinct centennial-scale temperature trends and insights into Pacific-wide climate impacts and teleconnections. Notably, the 20th century conditions, marked by simultaneous basin-scale warming and weak tropical Pacific zonal-meridional gradients, deviate from trends observed during the past six centuries. Combined with model simulations, our findings reveal that a weak SWCP gradient most markedly affects IPO-related rainfall patterns in the equatorial Pacific. Persistent synchronous western and central Pacific warming rates could lead to further drying climate across the Coral Sea region, adversely affecting Pacific Island nations.
dc.language.isoENen_US
dc.rightsAttribution-NonCommercial 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by-nc/3.0/us/*
dc.title.enCoral Sr/Ca-SST reconstruction from Fiji extending to ~1370 CE reveals insights into the Interdecadal Pacific Oscillation
dc.typeArticle de revueen_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalScience Advancesen_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
hal.identifierhal-04749443
hal.version1
hal.date.transferred2024-10-23T07:22:01Z
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exporttrue
dc.rights.ccCC BY-NCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Science%20Advances&rft.date=2024-08-14&rft.au=D%E2%80%99OLIVO,%20Juan%20P.&ZINKE,%20Jens&GOYAL,%20Rishav&ENGLAND,%20Matthew%20H.&PURICH,%20Ariaan&rft.genre=article


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