{"@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/1360004236558772224.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1175/jcli-d-15-0206.1"}},{"identifier":{"@type":"URI","@value":"http://journals.ametsoc.org/jcli/article-pdf/29/3/1237/4064690/jcli-d-15-0206_1.pdf"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Decadal Variation in Winter Mixed Layer Depth South of the Kuroshio Extension and Its Influence on Winter Mixed Layer Temperature"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n               <jats:p>The long-term behavior of the wintertime mixed layer depth (MLD) and mixed layer temperature (MLT) are investigated in a region south of the Kuroshio Extension (KE) (30°–37°N, 141°–155°E), an area of the North Pacific subtropical gyre where the deepest MLD occurs, using historical temperature profiles of 1968–2014. Both the MLD and MLT in March have low-frequency variations, which show significant decadal (~10 yr) variations after the late 1980s. Observational data and simulation outputs from a one-dimensional turbulent closure model reveal that surface cooling is the main control on winter MLD in the late 1970s and 1980s, whereas there is a change in the strength of subsurface stratification is the main control after ~1990. In the latter period, a weak (strong) subsurface stratification is caused by a straight path (convoluted path) of the KE and by a deepening (shallowing) of the main thermocline depth due to oceanic Rossby waves formed as a result of positive (negative) anomalies of wind stress curl associated with a southward (northward) movement of the Aleutian low in the central North Pacific. During deeper (shallower) periods of winter MLD, the strong (weak) vertical entrainment process, resulting from a rapid (slow) deepening of the mixed layer (ML) in January and February, forms a negative (positive) anomaly of temperature tendency. Consequently, the decadal variations in wintertime MLT are formed.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420282801198561152","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"50547320"},{"@type":"NRID","@value":"1000050547320"},{"@type":"NRID","@value":"9000257827293"},{"@type":"NRID","@value":"9000018773899"},{"@type":"NRID","@value":"9000317554934"},{"@type":"NRID","@value":"9000294329346"},{"@type":"NRID","@value":"9000398153730"},{"@type":"NRID","@value":"9000317555027"},{"@type":"NRID","@value":"9000018701207"},{"@type":"NRID","@value":"9000363504705"},{"@type":"NRID","@value":"9000414810874"},{"@type":"NRID","@value":"9000408498480"},{"@type":"NRID","@value":"9000016857176"},{"@type":"NRID","@value":"9000388467953"},{"@type":"NRID","@value":"9000019016307"},{"@type":"NRID","@value":"9000001984690"},{"@type":"NRID","@value":"9000023564479"},{"@type":"NRID","@value":"9000257767766"},{"@type":"NRID","@value":"9000414542099"},{"@type":"NRID","@value":"9000410296503"},{"@type":"NRID","@value":"9000018885881"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0145802"}],"foaf:name":[{"@value":"Shusaku Sugimoto"}],"jpcoar:affiliationName":[{"@value":"Frontier Research Institute for Interdisciplinary Sciences, Tohoku University, Sendai, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004236558772225","@type":"Researcher","foaf:name":[{"@value":"Shin’ichiro Kako"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Science and Engineering, Department of Ocean Civil Engineering, Kagoshima University, Kagoshima, Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"08948755"},{"@type":"EISSN","@value":"15200442"}],"prism:publicationName":[{"@value":"Journal of Climate"}],"dc:publisher":[{"@value":"American Meteorological Society"}],"prism:publicationDate":"2016-02-01","prism:volume":"29","prism:number":"3","prism:startingPage":"1237","prism:endingPage":"1252"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://journals.ametsoc.org/jcli/article-pdf/29/3/1237/4064690/jcli-d-15-0206_1.pdf"}],"createdAt":"2015-11-11","modifiedAt":"2020-12-07","project":[{"@id":"https://cir.nii.ac.jp/crid/1040282256839371776","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15K17756"},{"@type":"JGN","@value":"JP15K17756"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15K17756/"}],"notation":[{"@language":"ja","@value":"過去100年の亜熱帯モード水水温の構築：海洋温暖化評価と数十年周期変動機構解明"},{"@language":"en","@value":"Temperature of North Pacific subtropical mode water over the past 100 years: ocean warming and decadal-scale variations"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282677703188864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Variability of core layer temperature (CLT) of the North Pacific Subtropical Mode Water"}]},{"@id":"https://cir.nii.ac.jp/crid/1050282677733952768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Large-scale variabilities of wintertime wind stress curl field in the North Pacific and their relation to atmospheric teleconnection patterns"}]},{"@id":"https://cir.nii.ac.jp/crid/1050869456409859584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Southward Eddy Heat Transport Occurring along Southern Flanks of the Kuroshio Extension and the Gulf Stream in a 1/10° Global Ocean General Circulation 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