{"@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/1360011144068926720.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/98jc00263"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F98JC00263"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/98JC00263"}}],"dc:title":[{"@value":"On the western boundary currents in the Philippine Sea"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>In this study we describe the velocity structure and transport of the North Equatorial Current (NEC), the Kuroshio, and the Mindanao Current )MC( using repeated hydrographic sections near the Philippine coast. A most striking feature of the current system in the region is the undercurrent structure below the surface flow. Both the Luzon Undercurrent and the Mindanao Undercurrent appear to be permanent phenomena. The present data set also provides an estimate of the mean circulation diagram (relative to 1500 dbar) that involves a NEC transport of 41 Sverdrups (Sv), a Kuroshio transport of 14 Sv, and a MC transport of 27 Sv, inducing a mass balance better than 1 Sv within the region enclosed by stations. The circulation diagram is insensitive to vertical displacements of the reference level within the depth range between 1500 and 2500 dbar. Transport fluctuations are, in general, consistent with earlier observations; that is, the NEC and the Kuroshio vary in the same phase with a seasonal signal superimposed with interannual variations, and the transport of the MC is dominated by a quasi‐biennial oscillation. Dynamic height distributions are also examined to explore the dynamics of the current system.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380011144068926722","@type":"Researcher","foaf:name":[{"@value":"Tangdong Qu"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144068926721","@type":"Researcher","foaf:name":[{"@value":"Humio Mitsudera"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144068926720","@type":"Researcher","foaf:name":[{"@value":"Toshio Yamagata"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Oceans"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1998-04-15","prism:volume":"103","prism:number":"C4","prism:startingPage":"7537","prism:endingPage":"7548"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F98JC00263"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/98JC00263"}],"createdAt":"2004-02-04","modifiedAt":"2023-09-23","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360283691101478400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of the STCC eddies on the Kuroshio based on the 20-year JCOPE2 reanalysis results"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179757990272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ocean variability east of <scp>M</scp>indanao: Mooring observations at 7°N, revisited"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092882157056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Half-Century of Scientific Advancements Since the Cooperative Study of the Kuroshio and Adjacent Regions (CSK) Programme - Need for a new Kuroshio Research"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584340700291072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Natural and Anthropogenic Climate Variability Signals in a 237‐Year‐Long Coral Record From the Philippines"}]},{"@id":"https://cir.nii.ac.jp/crid/1360849942791398784","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Insight into Western Pacific Circulation from South China Sea Coral Skeletal Radiocarbon"}]},{"@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"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/98jc00263"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00513-3_references_DOI_XlLO2kSutXBOsABbKT4oPFwqOT8"},{"@type":"CROSSREF","@value":"10.1002/2015jc010703_references_DOI_XlLO2kSutXBOsABbKT4oPFwqOT8"},{"@type":"CROSSREF","@value":"10.1016/j.pocean.2021.102513_references_DOI_XlLO2kSutXBOsABbKT4oPFwqOT8"},{"@type":"CROSSREF","@value":"10.1029/2022pa004540_references_DOI_XlLO2kSutXBOsABbKT4oPFwqOT8"},{"@type":"CROSSREF","@value":"10.1017/rdc.2019.145_references_DOI_XlLO2kSutXBOsABbKT4oPFwqOT8"},{"@type":"CROSSREF","@value":"10.1016/j.pocean.2015.04.006_references_DOI_XlLO2kSutXBOsABbKT4oPFwqOT8"}]}