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Here, we present planktonic δ18O and Mg/Ca records from the western subtropical gyre of the North Pacific spanning the last 30 kyrs. The results indicate that subtropical SSTs were approximately 3°C lower during the last glacial than in the Holocene interglacial, indicating that glacial cooling occurred uniformly in the low to mid-latitudes of the western North Pacific. A decrease in intermediate depth temperatures at the late glacial suggests that the formation and/or advection of the subtropical mode water was enhanced due to a strong East Asian winter monsoon. The results suggest that the change in the thermal structure of the subtropical gyre was related to changes in East Asian monsoon activity."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004233286779650","@type":"Researcher","foaf:name":[{"@value":"Takuya Sagawa"}],"jpcoar:affiliationName":[{"@value":"Center for Advanced Marine Core Research; Kochi University; Nankoku Japan"},{"@value":"Senior Research Fellow Center; Ehime University; Matsuyama 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Ikehara"}],"jpcoar:affiliationName":[{"@value":"Center for Advanced Marine Core Research; Kochi University; Nankoku Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1420001326223989888","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"70448380"},{"@type":"NRID","@value":"1000070448380"},{"@type":"ORCID","@value":"0000-0002-7747-5421"},{"@type":"NRID","@value":"9000002546724"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/7000014814"}],"foaf:name":[{"@value":"Michinobu Kuwae"}],"jpcoar:affiliationName":[{"@value":"Senior Research Fellow Center; Ehime University; Matsuyama Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union 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