{"@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/1363388845417822720.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2008jc005213"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2008JC005213"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2008JC005213"}}],"dc:title":[{"@value":"Synoptic flow structures in the confluence region of the Kuroshio and the Ryukyu Current"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>In the southeastern region of Kyushu, Japan, the Kuroshio from the East China Sea encounters the Ryukyu Current from the east of the Ryukyu Islands. By analyzing synoptic sections of water properties and geostrophic velocity in August 2004 and October 2005, we distinguished the waters in the Kuroshio southeast of Kyushu to be separated into an offshore region and a shallow onshore one. The onshore water is derived from the East China Sea, while the offshore water originates from both the east of Amami‐Oshima Island and the interior region of the North Pacific. The water mass transport from the east of Amami‐Oshima Island may become equivalent to that of the Kuroshio in the East China Sea as in October 2005. The volume transport–averaged temperature of the Kuroshio southeast of Kyushu is significantly lower than that in the East China Sea because of the confluence with the colder Ryukyu Current east of the Amami‐Oshima Island.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388845417822723","@type":"Researcher","foaf:name":[{"@value":"Akira Nagano"}],"jpcoar:affiliationName":[{"@value":"Japan Agency for Marine‐Earth Science and Technology  Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388845417822720","@type":"Researcher","foaf:name":[{"@value":"Kaoru Ichikawa"}],"jpcoar:affiliationName":[{"@value":"Japan Agency for Marine‐Earth Science and Technology  Yokosuka Japan"},{"@value":"Research Institute for Applied Mechanics Kyushu University  Fukuoka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388845417822721","@type":"Researcher","foaf:name":[{"@value":"Hiroshi Ichikawa"}],"jpcoar:affiliationName":[{"@value":"Japan Agency for Marine‐Earth Science and Technology  Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388845417822722","@type":"Researcher","foaf:name":[{"@value":"Masanori Konda"}],"jpcoar:affiliationName":[{"@value":"Japan Agency for Marine‐Earth Science and Technology  Yokosuka Japan"},{"@value":"Department of Geophysics Kyoto University  Kyoto Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388845417822848","@type":"Researcher","foaf:name":[{"@value":"Kiyoshi Murakami"}],"jpcoar:affiliationName":[{"@value":"Nagasaki Marine Observatory Japan Meteorological Agency  Nagasaki Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Oceans"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2009-06","prism:volume":"114","prism:number":"C6","prism:startingPage":"C06007"},"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%2F2008JC005213"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2008JC005213"}],"createdAt":"2009-06-08","modifiedAt":"2023-10-12","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004231381686016","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Origin of near-surface high-salinity water observed in the Kuroshio Extension region"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025431138063104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Kuroshio Extension cold-core ring and wind drop-off observed in 2021–2022 winter"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302865717350656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Interannual sea-level variation around mainland Japan forced by subtropical North Pacific wind and its possible impact on the Tsugaru warm current"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848656311751552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Volume transports proceeding to the Kuroshio Extension region and recirculating in the Shikoku Basin"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861705571040128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"USV-Observed Turbulent Heat Flux Induced by Late Spring Cold Dry Air Incursion over Sub-Mesoscale Warm Regions off Sanriku, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367089652480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal vertical velocity variation in the western tropical Pacific and its relation to decadal ocean variability"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266981899520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Saildrone-observed atmospheric boundary layer response to winter mesoscale warm spot along the Kuroshio south of Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2008jc005213"},{"@type":"OPENAIRE","@value":"doi_dedup___::bf57fff5ea251449525fd411835e9fc3"},{"@type":"CROSSREF","@value":"10.1007/s10872-014-0237-5_references_DOI_Sb95IHTVnG14jrHrUQr8VxiCG83"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00513-3_references_DOI_Sb95IHTVnG14jrHrUQr8VxiCG83"},{"@type":"CROSSREF","@value":"10.1186/s40645-024-00649-4_references_DOI_Sb95IHTVnG14jrHrUQr8VxiCG83"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00358-8_references_DOI_Sb95IHTVnG14jrHrUQr8VxiCG83"},{"@type":"CROSSREF","@value":"10.1007/s10236-023-01580-w_references_DOI_Sb95IHTVnG14jrHrUQr8VxiCG83"},{"@type":"CROSSREF","@value":"10.1007/s10872-013-0173-9_references_DOI_Sb95IHTVnG14jrHrUQr8VxiCG83"},{"@type":"CROSSREF","@value":"10.3390/s22249695_references_DOI_Sb95IHTVnG14jrHrUQr8VxiCG83"}]}