{"@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/1361699994718778752.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1007/s10872-006-0007-0"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/s10872-006-0007-0.pdf"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/article/10.1007/s10872-006-0007-0/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/s10872-006-0007-0"}}],"dc:title":[{"@value":"Coastal Disturbance in Sea Level Propagating along the South Coast of Japan and Its Impact on the Kuroshio"}],"description":[{"notation":[{"@value":"The coastal sea level propagating westward along the south coast of Japan and the impact of the disturbance on the generation of the Kuroshio small meander have been examined. The propagation occurs in sea level variations for periods shorter than 10 days and is remarkable for periods of 4–6 days. Characteristics of the 4–6 day component have been studied using the extended empirical orthogonal function (EEOF). The first and second modes of EEOF are almost in-phase throughout the south coast of Japan. The higher four modes of EEOF are significantly excited when the Kuroshio takes the non-large-meander path, and propagate westward with phase speeds of 2.8 m s−1 (third and fourth modes) and 1.6 m s−1 (fifth and sixth modes) in the Kuroshio region west of Mera in the Boso Peninsula. The analysis shows that more than 70% of the small meanders generate in two months after a significant propagating disturbance reaches south of Kyushu when the velocity of the Kuroshio is high. This effect of coastal disturbance is examined by numerical experiments with a 2.5-layer model in which coastal disturbance is excited by vertical displacement of the upper interface. The result is that offshore displacement of the Kuroshio occurs southeast of Kyushu only in the case of significant upward displacement of the interface under the influence of a high Kuroshio velocity. The significant coastal disturbance, which is associated with upward displacement of the density interface, and a high Kuroshio velocity can therefore be important factors in generating small meanders."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699994718778752","@type":"Researcher","foaf:name":[{"@value":"Akira Nagano"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994718778753","@type":"Researcher","foaf:name":[{"@value":"Masaki Kawabe"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"09168370"},{"@type":"EISSN","@value":"1573868X"}],"prism:publicationName":[{"@value":"Journal of Oceanography"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2005-10","prism:volume":"61","prism:number":"5","prism:startingPage":"885","prism:endingPage":"903"},"reviewed":"false","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://link.springer.com/content/pdf/10.1007/s10872-006-0007-0.pdf"},{"@id":"http://link.springer.com/article/10.1007/s10872-006-0007-0/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1007/s10872-006-0007-0"}],"createdAt":"2006-01-26","modifiedAt":"2019-05-31","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360285706281184384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Bottom pressure change associated with the 2004–2005 large meander of the Kuroshio south of Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617879475584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seafloor Pressure Change Excited at the Northwest Corner of the Shikoku Basin by the Formation of the Kuroshio Large-Meander in September 2017"}]},{"@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/1360848656332489344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Characteristics of an atypical large-meander path of the Kuroshio current south of Japan formed in September 2017"}]},{"@id":"https://cir.nii.ac.jp/crid/1390585658888458112","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"2017年8月に発生した黒潮大蛇行の黒潮流路と日本南岸の潮位変動"},{"@language":"en","@value":"Sea-level variability on the south coast of Japan and the Kuroshio path during the 2017 Kuroshio large meander"},{"@language":"ja-Kana","@value":"2017ネン 8ガツ ニ ハッセイ シタ クロシオ ダイ ダコウ ノ クロシオ リュウロ ト ニホン ナンガン ノ チョウイ ヘンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845713068307328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Characteristics of temperature and current variations in the intermediate-deep layer of Oshima East Channel, Sagami Bay"},{"@language":"ja","@value":"相模湾大島東水道の中深層における水温・流速変動の特性"},{"@language":"ja-Kana","@value":"サガミワン オオシマ ヒガシスイドウ ノ チュウ シンソウ ニ オケル スイオン ・ リュウソク ヘンドウ ノ トクセイ"}]},{"@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":"10.1007/s10872-006-0007-0"},{"@type":"OPENAIRE","@value":"doi_dedup___::1340a810790882646bd19193a5c4406e"},{"@type":"CROSSREF","@value":"10.5928/kaiyou.22.1_1_references_DOI_4ykLMZ9137eSnlXZWU8zRNC15nP"},{"@type":"CROSSREF","@value":"10.1007/s10236-018-1169-1_references_DOI_4ykLMZ9137eSnlXZWU8zRNC15nP"},{"@type":"CROSSREF","@value":"10.3389/feart.2020.583481_references_DOI_4ykLMZ9137eSnlXZWU8zRNC15nP"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00358-8_references_DOI_4ykLMZ9137eSnlXZWU8zRNC15nP"},{"@type":"CROSSREF","@value":"10.1016/j.pocean.2021.102513_references_DOI_4ykLMZ9137eSnlXZWU8zRNC15nP"},{"@type":"CROSSREF","@value":"10.5928/kaiyou.34.3_81_references_DOI_4ykLMZ9137eSnlXZWU8zRNC15nP"},{"@type":"CROSSREF","@value":"10.1007/s11001-018-9372-5_references_DOI_4ykLMZ9137eSnlXZWU8zRNC15nP"}]}