{"@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/1361699996236661760.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2005gl022844"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2005GL022844"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005GL022844"}}],"dc:title":[{"@value":"North Pacific halocline and cold climate induced by Panamanian Gateway closure in a coupled ocean‐atmosphere GCM"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The influence of the closure of the Panamanian Gateway during the late Cenozoic on climate in and around the North Pacific is investigated by using a coupled ocean‐atmosphere general circulation model with an open and closed gateway. In the case of an open (closed) gateway, deep convection is present (absent) in the North Pacific. The deep convection is associated with surface saline water transported from the subtropical Atlantic through the open gateway to the North Pacific. On the other hand, with the closed gateway, the lack of saline water transport from the Atlantic induces halocline formation over the subarctic Pacific with cold climate. The deep convection in the North Pacific leads to a vigorous thermohaline circulation with larger meridional heat transport, and causes warmer climate in and around the North Pacific. These results are generally consistent with paleoceanographic and paleoclimatic estimates related to the closure of the Panamanian Gateway.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699996236661760","@type":"Researcher","foaf:name":[{"@value":"Tatsuo Motoi"}],"jpcoar:affiliationName":[{"@value":"Meteorological Research Institute Tsukuba Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380016867245757954","@type":"Researcher","foaf:name":[{"@value":"Wing‐Le Chan"}],"jpcoar:affiliationName":[{"@value":"Frontier Research Center for Global Change Japan Agency for Marine‐Earth Science and Technology Yokohama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380016867245757953","@type":"Researcher","foaf:name":[{"@value":"Shoshiro Minobe"}],"jpcoar:affiliationName":[{"@value":"Division of Earth and Planetary Sciences, Graduate School of Science Hokkaido University Sapporo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380016867245757952","@type":"Researcher","foaf:name":[{"@value":"Hiroshi Sumata"}],"jpcoar:affiliationName":[{"@value":"Division of Earth and Planetary Sciences, Graduate School of 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":"2005-05","prism:volume":"32","prism:number":"10","prism:startingPage":"L10618"},"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%2F2005GL022844"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005GL022844"}],"createdAt":"2005-05-27","modifiedAt":"2024-01-26","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 conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708408856704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Pliocene cooling enhanced by flow of low-salinity Bering Sea water to the Arctic Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679206497024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evolution of Large Scale Topography and Variation in Climate"},{"@language":"ja","@value":"大地形の変遷と気候変動"},{"@language":"ja-Kana","@value":"ダイチケイ ノ ヘンセン ト キコウ ヘンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266972605440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleoceanographic history of the Japan Sea over the last 9.5 million years inferred from radiolarian assemblages (IODP Expedition 346 Sites U1425 and U1430)"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2005gl022844"},{"@type":"OPENAIRE","@value":"doi_dedup___::5444d6acd034898d2848c788bfa824e6"},{"@type":"CROSSREF","@value":"10.5026/jgeography.117.1015_references_DOI_Qkdcc6UkO2MO1edpOKFOjx4rlrt"},{"@type":"CROSSREF","@value":"10.1038/ncomms8587_references_DOI_Qkdcc6UkO2MO1edpOKFOjx4rlrt"},{"@type":"CROSSREF","@value":"10.5194/cp-12-1619-2016_references_DOI_Qkdcc6UkO2MO1edpOKFOjx4rlrt"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0204-7_references_DOI_Qkdcc6UkO2MO1edpOKFOjx4rlrt"}]}