{"@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/1362825896359728000.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1112596"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1112596"}},{"identifier":{"@type":"NAID","@value":"30020399465"}}],"dc:title":[{"@value":"Permanent El Niño-Like Conditions During the Pliocene Warm Period"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>During the warm early Pliocene (∼4.5 to 3.0 million years ago), the most recent interval with a climate warmer than today, the eastern Pacific thermocline was deep and the average west-to-east sea surface temperature difference across the equatorial Pacific was only 1.5 ± 0.9°C, much like it is during a modern El Niño event. Thus, the modern strong sea surface temperature gradient across the equatorial Pacific is not a stable and permanent feature. Sustained El Niño-like conditions, including relatively weak zonal atmospheric (Walker) circulation, could be a consequence of, and play an important role in determining, global warmth.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825896359728001","@type":"Researcher","foaf:name":[{"@value":"Michael W. Wara"}],"jpcoar:affiliationName":[{"@value":"Ocean Sciences Department, University of California, Santa Cruz, CA 95064, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896359728000","@type":"Researcher","foaf:name":[{"@value":"Ana Christina Ravelo"}],"jpcoar:affiliationName":[{"@value":"Ocean Sciences Department, University of California, Santa Cruz, CA 95064, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896359728002","@type":"Researcher","foaf:name":[{"@value":"Margaret L. Delaney"}],"jpcoar:affiliationName":[{"@value":"Ocean Sciences Department, University of California, Santa Cruz, CA 95064, USA."}]}],"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":"2005-07-29","prism:volume":"309","prism:number":"5735","prism:startingPage":"758","prism:endingPage":"761"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1112596"}],"createdAt":"2005-06-24","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202542643456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sensitivity of Pliocene climate simulations in MRI-CGCM2.3 to respective boundary 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