{"@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/1363670318937125120.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.5194/os-5-303-2009"}},{"identifier":{"@type":"URI","@value":"https://os.copernicus.org/articles/5/303/2009/os-5-303-2009.pdf"}}],"dc:title":[{"@value":"The Kuroshio exchange with the South and East China Seas"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Abstract. The Kuroshio flows along the edges of the marginal East Asian seas such as the South China Sea (SCS) and East China Sea (ECS). Exchanges of materials and energy between the Kuroshio and the marginal seas partly control the environments of the marginal seas. In particular, saline water from the Kuroshio maintains certain salinity in the shelf water in the ECS. Nutrients from the subsurface of the Kuroshio may influence primary production on the shelf. We summarize how the Kuroshio comes into contact with the shelf water or marginal seas, describing phenomena related to the exchange between the Kuroshio and the ECS along with the SCS, using reports in the literature along with original data. The Kuroshio tends to intrude into the SCS through the Luzon Strait in various manners such as direct intrusion, associated with eddies and as a loop current. The Kuroshio intrusion into the shelf region of the ECS has distinct seasonal variation and the Taiwan Warm Current plays a significant role in the determination of water properties in the outer shelf associated with the Kuroshio intrusion. We then examine physical processes related to the interaction between the Kuroshio and shelf water. Interaction between the Kuroshio and the bottom topography is an important process in the control of the exchange around the shelf break. Vertical mixing and frontal eddies are also important factors that control the water exchange and formation of water masses in the outer shelf. Wind stress plays a significant role in the exchange with a rather event-like manner. To determine the source of the water masses, chemical tracers could be powerful tools and it is suggested that a significant part of the shelf water consists of Kuroshio intermediate water.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380285711831106181","@type":"Researcher","foaf:name":[{"@value":"T. Matsuno"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318937125121","@type":"Researcher","foaf:name":[{"@value":"J.-S. Lee"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318937125122","@type":"Researcher","foaf:name":[{"@value":"S. Yanao"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"18120792"}],"prism:publicationName":[{"@value":"Ocean Science"}],"dc:publisher":[{"@value":"Copernicus GmbH"}],"prism:publicationDate":"2009-08-03","prism:volume":"5","prism:number":"3","prism:startingPage":"303","prism:endingPage":"312"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://creativecommons.org/licenses/by/3.0/"],"url":[{"@id":"https://os.copernicus.org/articles/5/303/2009/os-5-303-2009.pdf"}],"createdAt":"2010-04-29","modifiedAt":"2025-02-15","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=G","dc:title":"G"},{"@id":"https://cir.nii.ac.jp/all?q=Environmental%20sciences","dc:title":"Environmental sciences"},{"@id":"https://cir.nii.ac.jp/all?q=Geography.%20Anthropology.%20Recreation","dc:title":"Geography. Anthropology. Recreation"},{"@id":"https://cir.nii.ac.jp/all?q=GE1-350","dc:title":"GE1-350"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050856995323638400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Eddy-driven nutrient transport and associated upper-ocean primary production along the Kuroshio"},{"@value":"Eddy‐driven nutrient transport and associated upper‐ocean primary production along the<scp>K</scp>uroshio"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182042634752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Variability in nitrogen sources for new production in the vicinity of the shelf edge of the East China Sea in summer"}]},{"@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/1360864422598425216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Review of oceanic mesoscale processes in the North Pacific: Physical and biogeochemical impacts"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205320294528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"黒潮と内部波が影響する伊豆諸島周辺海域における流動場の解明"},{"@language":"en","@value":"A STUDY OF FLOW FIELD INFLUENCED BY INTERNAL TIDES AND THE KUROSHIO AROUND THE IZU-CHAIN ISLANDS"},{"@language":"ja-Kana","@value":"クロシオ ト ナイブハ ガ エイキョウ スル イズ ショトウ シュウヘン カイイキ ニ オケル リュウドウジョウ ノ カイメイ"},{"@value":"黒潮周辺海域における海洋変動に対する一次生産応答の季節変動特性について"},{"@language":"ja-Kana","@value":"クロシオ シュウヘン カイイキ ニ オケル カイヨウ ヘンドウ ニ タイスル イチジ セイサン オウトウ ノ キセツ ヘンドウ トクセイ ニ ツイテ"},{"@value":"BIOGEOCHEMICAL RESPONSES TO SEASONAL OCEANIC VARIABILITY AROUND THE KUROSHIO ANALYZED USING A ROMS-NPZD MODEL"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288070384896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"北太平洋乱流ホットスポットでの鉛直混合強度の観測的知見"},{"@language":"en","@value":"A brief review of vertical mixing observations at mixing hotspots in the North Pacific"},{"@language":"ja-Kana","@value":"キタタイヘイヨウ ランリュウ ホットスポット デ ノ エンチョク コンゴウ キョウド ノ カンソクテキ チケン"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417113179136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleoceanographic changes in the Northern East China Sea during the last 400 kyr as inferred from radiolarian assemblages (IODP Site U1429)"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.5194/os-5-303-2009"},{"@type":"OPENAIRE","@value":"doi_dedup___::67c3bd2adfe5efe9295fce108d5d9fc0"},{"@type":"CROSSREF","@value":"10.1016/j.csr.2013.04.014_references_DOI_aE7pdqMOTRBNvcwyrdcZ5pH9HKG"},{"@type":"CROSSREF","@value":"10.1002/2017jc012847_references_DOI_aE7pdqMOTRBNvcwyrdcZ5pH9HKG"},{"@type":"CROSSREF","@value":"10.1186/s40645-019-0256-3_references_DOI_aE7pdqMOTRBNvcwyrdcZ5pH9HKG"},{"@type":"CROSSREF","@value":"10.1016/j.pocean.2021.102513_references_DOI_aE7pdqMOTRBNvcwyrdcZ5pH9HKG"},{"@type":"CROSSREF","@value":"10.5928/kaiyou.26.5_151_references_DOI_aE7pdqMOTRBNvcwyrdcZ5pH9HKG"},{"@type":"CROSSREF","@value":"10.1016/j.pocean.2022.102955_references_DOI_aE7pdqMOTRBNvcwyrdcZ5pH9HKG"},{"@type":"CROSSREF","@value":"10.2208/kaigan.73.i_457_references_DOI_aE7pdqMOTRBNvcwyrdcZ5pH9HKG"}]}