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The cooling by 5°C from 21 ka to 12.8 ka implies the equatorward shift of the subarctic boundary in the northwestern Pacific by ∼2.8° in latitude. This shift was a result of the stronger summer Okhotsk High. The Okhotsk High was likely enhanced by the combined effects of El Niño‐like conditions in the tropical Pacific and the heating of the land surface of northeastern Siberia.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420564276176030080","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"60332475"},{"@type":"NRID","@value":"1000060332475"},{"@type":"NRID","@value":"9000003877150"},{"@type":"NRID","@value":"9000283907664"},{"@type":"NRID","@value":"9000347188342"},{"@type":"NRID","@value":"9000021915697"},{"@type":"NRID","@value":"9000283907193"},{"@type":"NRID","@value":"9000258408228"},{"@type":"NRID","@value":"9000347082388"},{"@type":"NRID","@value":"9000370281521"},{"@type":"NRID","@value":"9000345426484"},{"@type":"NRID","@value":"9000254697972"},{"@type":"NRID","@value":"9000370253677"},{"@type":"NRID","@value":"9000283908562"},{"@type":"NRID","@value":"9000283904412"},{"@type":"NRID","@value":"9000254631029"},{"@type":"NRID","@value":"9000019247780"},{"@type":"NRID","@value":"9000283907622"},{"@type":"NRID","@value":"9000283907048"},{"@type":"NRID","@value":"9000239511777"},{"@type":"NRID","@value":"9000390890972"},{"@type":"NRID","@value":"9000283905296"},{"@type":"NRID","@value":"9000254631187"},{"@type":"NRID","@value":"9000253227655"},{"@type":"NRID","@value":"9000368412052"},{"@type":"NRID","@value":"9000415205565"},{"@type":"NRID","@value":"9000384265564"},{"@type":"NRID","@value":"9000399524298"},{"@type":"NRID","@value":"9000254631341"},{"@type":"NRID","@value":"9000258406176"},{"@type":"NRID","@value":"9000241122176"},{"@type":"NRID","@value":"9000242124612"},{"@type":"NRID","@value":"9000254579558"},{"@type":"NRID","@value":"9000237765738"},{"@type":"NRID","@value":"9000283905338"},{"@type":"NRID","@value":"9000410515527"},{"@type":"NRID","@value":"9000257917737"},{"@type":"NRID","@value":"9000283907207"},{"@type":"NRID","@value":"9000242690973"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0073964"}],"foaf:name":[{"@value":"Masanobu Yamamoto"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Environmental Earth Science Hokkaido University  Sapporo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380861293149034240","@type":"Researcher","foaf:name":[{"@value":"Ryutaro Suemune"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Environmental Earth Science Hokkaido University  Sapporo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380861293149034241","@type":"Researcher","foaf:name":[{"@value":"Tadamichi Oba"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Environmental Earth Science Hokkaido University  Sapporo Japan"}]}],"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":"2005-03","prism:volume":"32","prism:number":"5","prism:startingPage":"L05609"},"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%2F2004GL021903"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2004GL021903"}],"createdAt":"2005-03-08","modifiedAt":"2023-10-31","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=452","dc:title":"452"}],"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 Atlantic"},{"@value":"Millennial-scale hydrographic changes in the 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section, central Japan: a reference for the Early-Middle Pleisotocene boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1050587981430434048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Climate reconstruction based on GDGT-based proxies in a paleosol sequence in Japan: Postdepositional effect on the estimation of air temperature"}]},{"@id":"https://cir.nii.ac.jp/crid/1050869456410343808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Intense winter cooling of the surface water in the northern Okinawa Trough during the last glacial period"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233286387840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Variations of East Asian summer monsoon since the last deglaciation based 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