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Cited 69 time in webofscience Cited 74 time in scopus
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dc.contributor.authorMagdalena Andres-
dc.contributor.authorKIM, KUH-
dc.date.accessioned2016-04-01T02:53:05Z-
dc.date.available2016-04-01T02:53:05Z-
dc.date.created2010-05-18-
dc.date.issued2009-08-28-
dc.identifier.issn0094-8276-
dc.identifier.other2009-OAK-0000021281-
dc.identifier.urihttps://oasis.postech.ac.kr/handle/2014.oak/25927-
dc.description.abstractPacific Decadal Oscillation (PDO) index is strongly correlated with vertically integrated transport carried by the Kuroshio through the East China Sea (ECS). Transport was determined from satellite altimetry calibrated with in situ data and its correlation with PDO index (0.76) is highest at zero lag. Total PDO-correlated transport variation carried by the ECS-Kuroshio and Ryukyu Current is about 4 Sv. In addition, PDO index is strongly negatively correlated, at zero lag, with NCEP wind-stress-curl over the central North Pacific at ECS latitudes. Sverdrup transport, calculated from wind-stress-curl anomalies, is consistent with the observed transport variations. Finally, PDO index and ECS-Kuroshio transport are each negatively correlated with Kuroshio Position Index in the Tokara Strait; this can be explained by a model in which Kuroshio path is steered by topography when transport is low and is inertially controlled when transport is high. Citation: Andres, M., J.-H. Park, M. Wimbush, X.-H. Zhu, H. Nakamura, K. Kim, and K.-I. Chang (2009), Manifestation of the Pacific Decadal Oscillation in the Kuroshio, Geophys. Res. Lett., 36, L16602, doi:10.1029/2009GL039216.-
dc.description.statementofresponsibilityX-
dc.languageEnglish-
dc.publisherAmerica Geophysical Union-
dc.relation.isPartOfGEOPHYSICAL RESEARCH LETTERS-
dc.titleManifestation of the Pacific Decadal Oscillation in the Kuroshio-
dc.typeArticle-
dc.contributor.college환경공학부-
dc.identifier.doi10.1029/2009GL039216-
dc.author.googleAndres, M-
dc.author.googlePark, JH-
dc.author.googleWimbush, M-
dc.author.googleZhu, XH-
dc.author.googleNakamura, H-
dc.author.googleKim, K-
dc.author.googleChang, KI-
dc.relation.volume36-
dc.relation.startpageL16602-
dc.relation.lastpageL16602-
dc.contributor.id10051591-
dc.relation.journalGEOPHYSICAL RESEARCH LETTERS-
dc.relation.indexSCI급, SCOPUS 등재논문-
dc.relation.sciSCI-
dc.collections.nameJournal Papers-
dc.type.rimsART-
dc.identifier.bibliographicCitationGEOPHYSICAL RESEARCH LETTERS, v.36, pp.L16602 - L16602-
dc.identifier.wosid000269348800001-
dc.date.tcdate2019-02-01-
dc.citation.endPageL16602-
dc.citation.startPageL16602-
dc.citation.titleGEOPHYSICAL RESEARCH LETTERS-
dc.citation.volume36-
dc.contributor.affiliatedAuthorKIM, KUH-
dc.identifier.scopusid2-s2.0-71949094725-
dc.description.journalClass1-
dc.description.journalClass1-
dc.description.wostc29-
dc.type.docTypeArticle-
dc.subject.keywordPlusSATELLITE-ALTIMETER-
dc.subject.keywordPlusNORTH PACIFIC-
dc.subject.keywordPlusSEA-LEVEL-
dc.subject.keywordPlusVARIABILITY-
dc.subject.keywordPlusEXTENSION-
dc.subject.keywordPlusCIRCULATION-
dc.relation.journalWebOfScienceCategoryGeosciences, Multidisciplinary-
dc.description.journalRegisteredClassscie-
dc.description.journalRegisteredClassscopus-
dc.relation.journalResearchAreaGeology-

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김구KIM, KUH
POSTECH Ocean Science & Tech Institute
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