{"@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/1361137043885401344.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2002jc001590"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2002JC001590"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2002JC001590"}},{"identifier":{"@type":"NAID","@value":"30013329685"}}],"dc:title":[{"@value":"Distribution and formation of Okhotsk Sea Intermediate Water: An analysis of isopycnal climatological data"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>In order to clarify the distribution and formation of Okhotsk Sea Intermediate Water (OSIW) an isopycnal climatological data set based on all of the available historical observations is developed and examined. The isopycnal maps clearly show that there are two direct ventilation sources for OSIW: Dense Shelf Water (DSW) with cold and fresh properties influenced by sea ice formation in the northwest shelf region and Forerunner of Soya Warm Current Water (FSCW), which has warm and saline properties originating in the Japan Sea. The cold and fresh water extends southward from the northwest shelf to the shelf slope off Sakhalin Island. It suggests that DSW is transported southward by the East Sakhalin Current. The DSW enters the Kuril Basin and mixes with FSCW and Western Subarctic Water (WSAW) originating from the North Pacific to form OSIW. The annual mean production rate of DSW estimated from the total volume of DSW over the shelf in spring and summer is 0.67 Sv (1 Sv = 10<jats:sup>6</jats:sup> m<jats:sup>3</jats:sup>/s). The annual mean volume transport of FSCW is estimated to be 0.08 Sv on the basis of its cross‐section area and the current speed. Assumption of isopycnal mixing yields a mixing ratio of 1:1:0.1 among DSW, WSAW, and FSCW to form OSIW. We estimate the annual production rate of OSIW to be 1.4 Sv; the corresponding OSIW's renewal time is 7 years. Continued assumption of isopycnal mixing yields a mixing ratio of 0.6:0.4 between WSAW and OSIW to form Oyashio Intermediate Water (OYIW).</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137043885401344","@type":"Researcher","foaf:name":[{"@value":"Motoyo Itoh"}],"jpcoar:affiliationName":[{"@value":"Japan Marine Science and Technology Center  Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298344356895232","@type":"Researcher","foaf:name":[{"@value":"Kay I. Ohshima"}],"jpcoar:affiliationName":[{"@value":"Institute of Low Temperature Science Hokkaido University  Sapporo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298344356895233","@type":"Researcher","foaf:name":[{"@value":"Masaaki Wakatsuchi"}],"jpcoar:affiliationName":[{"@value":"Institute of Low Temperature Science Hokkaido University  Sapporo Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Oceans"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2003-08","prism:volume":"108","prism:number":"C8","prism:startingPage":"3258"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2002JC001590"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2002JC001590"}],"createdAt":"2003-08-12","modifiedAt":"2023-10-14","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050025031481843712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Simulations of chlorofluorocarbons in and around the Sea of Okhotsk : Effects of tidal mixing and brine rejection on the ventilation"},{"@value":"Oceanic iron supply mechanisms which support the spring diatom bloom in the Oyashio region, western subarctic Pacific"},{"@value":"Mechanisms 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海洋生態系に関わる親潮・黒潮海域の水塊と変動に関する研究"},{"@language":"ja-Kana","@value":"2011ネンド ニホン カイヨウ ガッカイ オカダショウ ジュショウ キネン ロンブン カイヨウ セイタイケイ ニ カカワル オヤシオ ・ クロシオ カイイキ ノ スイカイ ト ヘンドウ ニ カンスル ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763048510208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"北太平洋亜寒帯における鉄の供給過程"},{"@language":"en","@value":"Iron supply to the subarctic North Pacific"},{"@language":"ja-Kana","@value":"キタタイヘイヨウ アカンタイ ニ オケル テツ ノ キョウキュウ カテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390290493077840896","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Transport and modification processes of dense Soya Current Water in the boundary region between shelf and basin areas off Abashiri"},{"@language":"ja","@value":"網走沖の陸棚ー海盆境界域におけるdense Soya Current Waterの輸送と変質過程"},{"@language":"ja-Kana","@value":"アバシリオキ ノ リクダナ-カイボン キョウカイイキ ニ オケル dense Soya Current 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