{"@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/1363388846213553792.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.aat9393"}},{"identifier":{"@type":"URI","@value":"https://syndication.highwire.org/content/doi/10.1126/science.aat9393"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.aat9393"}}],"dc:title":[{"@value":"East Asian hydroclimate modulated by the position of the westerlies during Termination I"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>East Asian monsoon mysteries</jats:title>\n          <jats:p>\n            What exactly does the oxygen isotopic composition of speleothems tell us about the East Asian monsoon? They provide magnificent, detailed records of hydroclimate, but precisely what aspects of hydroclimate they record is unclear. Zhang\n            <jats:italic>et al.</jats:italic>\n            present data from two speleothems from central eastern China for the period from 21,000 to 10,000 years ago and suggest that the cause of the oxygen isotopic variability that they observe is more complex than simple changes in monsoon strength or intensity (see the Perspective by McGee). Alternatively, this variation may reflect the lengths of various phases of the monsoon and the regional heterogeneity of the East Asian hydroclimate.\n          </jats:p>\n          <jats:p>\n            <jats:italic>Science</jats:italic>\n            , this issue p.\n            <jats:related-article xmlns:xlink=\"http://www.w3.org/1999/xlink\" ext-link-type=\"doi\" issue=\"6414\" page=\"580\" related-article-type=\"in-this-issue\" vol=\"362\" xlink:href=\"10.1126/science.aat9393\">580</jats:related-article>\n            ; see also p.\n            <jats:related-article xmlns:xlink=\"http://www.w3.org/1999/xlink\" ext-link-type=\"doi\" issue=\"6414\" page=\"518\" related-article-type=\"in-this-issue\" vol=\"362\" xlink:href=\"10.1126/science.aav5280\">518</jats:related-article>\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380853567687974538","@type":"Researcher","foaf:name":[{"@value":"Hongbin Zhang"}],"jpcoar:affiliationName":[{"@value":"State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China."},{"@value":"State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, 430074, China."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846213553801","@type":"Researcher","foaf:name":[{"@value":"Michael L. Griffiths"}],"jpcoar:affiliationName":[{"@value":"Department of Environmental Science, William Paterson University, Wayne, NJ 07470, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846213553797","@type":"Researcher","foaf:name":[{"@value":"John C. H. Chiang"}],"jpcoar:affiliationName":[{"@value":"Department of Geography and Berkeley Atmospheric Sciences Center, University of California, Berkeley, CA 94720, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846213553794","@type":"Researcher","foaf:name":[{"@value":"Wenwen Kong"}],"jpcoar:affiliationName":[{"@value":"Department of Geography and Berkeley Atmospheric Sciences Center, University of California, Berkeley, CA 94720, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846213553792","@type":"Researcher","foaf:name":[{"@value":"Shitou Wu"}],"jpcoar:affiliationName":[{"@value":"Department of Geochemistry, Faculty of Geoscience and Geography, Georg-August University Goettingen, Goettingen 37077, Germany."},{"@value":"Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846213553795","@type":"Researcher","foaf:name":[{"@value":"Alyssa Atwood"}],"jpcoar:affiliationName":[{"@value":"Department of Geography and Berkeley Atmospheric Sciences Center, University of California, Berkeley, CA 94720, USA."},{"@value":"School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846213553798","@type":"Researcher","foaf:name":[{"@value":"Junhua Huang"}],"jpcoar:affiliationName":[{"@value":"State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, 430074, China."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846213553796","@type":"Researcher","foaf:name":[{"@value":"Hai Cheng"}],"jpcoar:affiliationName":[{"@value":"Institute of Global Environmental Change, Xi’an Jiaotong University, Xi’an, 710049, China."},{"@value":"Department of Earth Science, University of Minnesota, Minneapolis, MN 55455, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846213553799","@type":"Researcher","foaf:name":[{"@value":"Youfeng Ning"}],"jpcoar:affiliationName":[{"@value":"Institute of Global Environmental Change, Xi’an Jiaotong University, Xi’an, 710049, China."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846213553800","@type":"Researcher","foaf:name":[{"@value":"Shucheng Xie"}],"jpcoar:affiliationName":[{"@value":"State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China."},{"@value":"Department of Geography, School of Earth Sciences, China University of Geosciences, Wuhan, 430074, China."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00368075"},{"@type":"EISSN","@value":"10959203"}],"prism:publicationName":[{"@value":"Science"}],"dc:publisher":[{"@value":"American Association for the Advancement of Science (AAAS)"}],"prism:publicationDate":"2018-11-02","prism:volume":"362","prism:number":"6414","prism:startingPage":"580","prism:endingPage":"583"},"reviewed":"false","url":[{"@id":"https://syndication.highwire.org/content/doi/10.1126/science.aat9393"},{"@id":"https://www.science.org/doi/pdf/10.1126/science.aat9393"}],"createdAt":"2018-11-01","modifiedAt":"2024-01-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360567182975326208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Aeolian delivery to Ulleung Basin, Korea (Japan Sea), during development of the East Asian Monsoon through the last 12 Ma"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584340719927168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sahara’s surface transformation forced an abrupt hydroclimate decline and Neolithic culture transition in northern China"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417114562560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Millennial-scale variability of East Asian summer monsoon inferred from sea surface salinity in the northern East China Sea (ECS) and its impact on the Japan Sea during Marine Isotope Stage (MIS) 3"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1126/science.aat9393"},{"@type":"CROSSREF","@value":"10.1017/s001675681900013x_references_DOI_6CG8hQRMOYmYUiLKNRoshBT5mwX"},{"@type":"CROSSREF","@value":"10.1016/j.xinn.2023.100550_references_DOI_6CG8hQRMOYmYUiLKNRoshBT5mwX"},{"@type":"CROSSREF","@value":"10.1186/s40645-019-0283-0_references_DOI_6CG8hQRMOYmYUiLKNRoshBT5mwX"}]}