{"@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/1360292619087797632.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.csr.2010.05.003"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S027843431000169X?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S027843431000169X?httpAccept=text/plain"}}],"dc:title":[{"@value":"Response of a summertime anticyclonic eddy to wind forcing in Funka Bay, Hokkaido, Japan"}],"description":[{"notation":[{"@value":"Abstract   Flow fluctuations inside an anticyclonic eddy in summertime Funka Bay were examined using three moorings and hydrographic data. The flow pattern above a sharp pycnocline with a concave isopycnal structure during the mooring period was characterized by high mean kinetic energy and relatively low eddy kinetic energy. The ratios of eddy to mean kinetic energy were equal to or less than one, and the mean flow field and isopycnal structure indicated the existence of a stable anticyclonic eddy above the sharp pycnocline under approximate geostrophic balance. Larger flow fluctuations with periods longer than 7 days were dominant inside the eddy. The low-frequency flow fluctuations are accompanied by north to northeastward movement of the eddy with deepening of the pycnocline and spin-up of the anticyclonic circulation. The wind field over Funka Bay is characterized by bay-scale wind fluctuations. The bay-scale winds are greatly influenced by the land topography around Funka Bay, resulting in non-uniform structure with significant wind stress curl. The bay-scale wind fluctuations are termed “locally modified wind” in the present study. The locally modified wind has a negative (positive) wind stress curl in the central–northeastern (southwestern) region of Funka Bay. The north to northeastward movement of the eddy is caused by horizontal non-uniform supply of vorticity from the locally modified wind forcing by the Ekman pumping process. Through this process, the anticyclonic circulation is enhanced (weakened) in the central–northeastern (southwestern) part of the eddy, resulting in the eddy moving north to northeastward with the pycnocline deepening and spin-up of the anticyclonic circulation. The locally modified wind forcing induces low-frequency flow fluctuations through the movement of the eddy in summertime Funka Bay."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380292619087797633","@type":"Researcher","foaf:name":[{"@value":"Daisuke Takahashi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380292619087797761","@type":"Researcher","foaf:name":[{"@value":"Hideo Miyake"}]},{"@id":"https://cir.nii.ac.jp/crid/1380292619087797634","@type":"Researcher","foaf:name":[{"@value":"Takeyasu Nakayama"}]},{"@id":"https://cir.nii.ac.jp/crid/1380292619087797762","@type":"Researcher","foaf:name":[{"@value":"Naoto Kobayashi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380292619087797760","@type":"Researcher","foaf:name":[{"@value":"Kazuo Kido"}]},{"@id":"https://cir.nii.ac.jp/crid/1380292619087797632","@type":"Researcher","foaf:name":[{"@value":"Yoshinori Nishida"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"02784343"}],"prism:publicationName":[{"@value":"Continental Shelf Research"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2010-07","prism:volume":"30","prism:number":"13","prism:startingPage":"1435","prism:endingPage":"1449"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S027843431000169X?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S027843431000169X?httpAccept=text/plain"}],"createdAt":"2010-05-22","modifiedAt":"2025-10-03","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360565165850553600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Influence of hydrography on the spatiotemporal variability of phytoplankton assemblages and primary productivity in Funka Bay and the Tsugaru Strait"}]},{"@id":"https://cir.nii.ac.jp/crid/1390002184862535680","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Numerical experiments of surface clockwise circulation in Funka Bay during early summer"},{"@language":"ja","@value":"初夏の噴火湾表層時計回り水平循環流の数値実験"},{"@language":"ja-Kana","@value":"ショカ ノ フンカワン ヒョウソウ ドケイ マワリ スイヘイ ジュンカンリュウ ノ スウチ ジッケン"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892137572992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The role of snowmelt runoff on the ocean environment and scallop production in Funka Bay, Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.csr.2010.05.003"},{"@type":"OPENAIRE","@value":"doi_dedup___::259d70cc94c23c70f9efb18938cc19b4"},{"@type":"CROSSREF","@value":"10.5928/kaiyou.28.4-5-6_51_references_DOI_a0RMNtO0XnmuORY7dfi6LL3CmkP"},{"@type":"CROSSREF","@value":"10.1186/s40645-014-0025-2_references_DOI_a0RMNtO0XnmuORY7dfi6LL3CmkP"},{"@type":"CROSSREF","@value":"10.1016/j.ecss.2017.02.019_references_DOI_a0RMNtO0XnmuORY7dfi6LL3CmkP"}]}