{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1360004233286754048.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2010gl045202"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2010GL045202"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2010GL045202"}},{"identifier":{"@type":"HANDLE","@value":"1912/4288"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Dynamic millennial‐scale climate changes in the northwestern Pacific over the past 40,000 years"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Ice core records of polar temperatures and greenhouse gases document abrupt millennial‐scale oscillations that suggest the reduction or shutdown of thermohaline Circulation (THC) in the North Atlantic Ocean may induce the abrupt cooling in the northern hemisphere. It remains unknown, however, whether the sea surface temperature (SST) is cooling or warming in the Kuroshio of the Northwestern Pacific during the cooling event. Here we present an AMS <jats:sup>14</jats:sup>C‐dated foraminiferal Mg/Ca SST record from the central Okinawa Trough and document that the SST variations exhibit two steps of warming since 21 ka — at 14.7 ka and 12.8 ka, and a cooling (∼1.5°C) during the interval of the Younger Dryas. By contrast, we observed no SST change or oceanic warming (∼1.5–2°C) during the episodes of Northern Hemisphere cooling between ∼21–40 ka. We therefore suggest that the “Antarctic‐like” timing and amplitude of millennial‐scale SST variations in the subtropical Northwestern Pacific between 20–40 ka may have been determined by rapid ocean adjustment processes in response to abrupt wind stress and meridional temperature gradient changes in the North Pacific.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380579812932255360","@type":"Researcher","foaf:name":[{"@value":"M.‐T. Chen"}],"jpcoar:affiliationName":[{"@value":"Institute of Applied Geosciences National Taiwan Ocean University  Keelung Taiwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233286754058","@type":"Researcher","foaf:name":[{"@value":"X. P. Lin"}],"jpcoar:affiliationName":[{"@value":"Physical Oceanography Laboratory Ocean University of China  Qingdao China"}]},{"@id":"https://cir.nii.ac.jp/crid/1380579812932255363","@type":"Researcher","foaf:name":[{"@value":"Y.‐P. Chang"}],"jpcoar:affiliationName":[{"@value":"Institute of Applied Geosciences National Taiwan Ocean University  Keelung Taiwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380579812932255362","@type":"Researcher","foaf:name":[{"@value":"Y.‐C. Chen"}],"jpcoar:affiliationName":[{"@value":"Institute of Applied Geosciences National Taiwan Ocean University  Keelung Taiwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233286754187","@type":"Researcher","foaf:name":[{"@value":"L. Lo"}],"jpcoar:affiliationName":[{"@value":"Department of Geosciences National Taiwan University  Taipei Taiwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380579812932255361","@type":"Researcher","foaf:name":[{"@value":"C.‐C. Shen"}],"jpcoar:affiliationName":[{"@value":"Department of Geosciences National Taiwan University  Taipei Taiwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233286754053","@type":"Researcher","foaf:name":[{"@value":"Y. Yokoyama"}],"jpcoar:affiliationName":[{"@value":"Atmosphere and Ocean Research Institute and Department of Earth and Planetary Sciences University of Tokyo  Kashiwanoha Japan"},{"@value":"Institute of Biogeosciences, Japan Agency for Marine‐Earth Science and Technology  Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233286753922","@type":"Researcher","foaf:name":[{"@value":"D. W. Oppo"}],"jpcoar:affiliationName":[{"@value":"Department of Geology and Geophysics Woods Hole Oceanographic Institution  Woods Hole Massachusetts USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233286753921","@type":"Researcher","foaf:name":[{"@value":"W. G. Thompson"}],"jpcoar:affiliationName":[{"@value":"Department of Geology and Geophysics Woods Hole Oceanographic Institution  Woods Hole Massachusetts USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233286754181","@type":"Researcher","foaf:name":[{"@value":"R. Zhang"}],"jpcoar:affiliationName":[{"@value":"Geophysical Fluid Dynamics Laboratory, NOAA  Princeton New Jersey USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2010-12","prism:volume":"37","prism:number":"23","prism:startingPage":"L23603"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2010GL045202"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2010GL045202"}],"createdAt":"2010-12-02","modifiedAt":"2023-10-30","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Mg/Ca","dc:title":"Mg/Ca"},{"@id":"https://cir.nii.ac.jp/all?q=Oxygen%20isotope","dc:title":"Oxygen isotope"},{"@id":"https://cir.nii.ac.jp/all?q=Sea%20surface%20temperature","dc:title":"Sea surface temperature"},{"@id":"https://cir.nii.ac.jp/all?q=Kuroshio","dc:title":"Kuroshio"},{"@id":"https://cir.nii.ac.jp/all?q=East%20Asian%20monsoon","dc:title":"East Asian monsoon"},{"@id":"https://cir.nii.ac.jp/all?q=551","dc:title":"551"},{"@id":"https://cir.nii.ac.jp/all?q=Pacific","dc:title":"Pacific"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040282257418447104","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"18101001"},{"@type":"JGN","@value":"JP18101001"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-18101001/"}],"notation":[{"@language":"ja","@value":"近未来予測のための古海洋学:温暖化に伴う気候モードジャンプの可能性"},{"@language":"en","@value":"Paleoceanography for future prediction : a possibility of climate mode jump with global warming"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050002213761277952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Millennial-scale hydrographic changes in the northwestern Pacific during marine isotope stage 19: teleconnections with ice melt in the North 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