{"@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/1362262943961681664.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2008gl035040"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2008GL035040"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2008GL035040"}}],"dc:title":[{"@value":"Ocean physical and biogeochemical responses to the passage of Typhoon Meari in the East China Sea observed from Argo float and multiplatform satellites"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We elucidated ocean physical and biogeochemical responses to slow‐moving Typhoon Meari using a new method combining Argo float and satellite observations. Meari‐driven upwelling brought colder, nutrient‐rich deep water to the surface layer, causing sea surface cooling (3–6°C) and threefold enhancement of primary production (PP). Maximum surface cooling (and hence nutrient injection) and peak PP enhancement lagged Meari's passage by 1 and 3 days, respectively, implying that remarkable PP enhancement was attributed to new production (NP). This NP accounted for approximately 3.8% of annual carbon export in the East China Sea (ECS) outer shelf, suggesting that typhoon‐driven upwelling is important for biogeochemical processes in the ECS. Given the wide coverage of Argo float and satellite data, our new approach may prompt comparative studies in other basins and advance the understanding of the role of tropical cyclones in the global ocean biogeochemical cycle.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262943961681536","@type":"Researcher","foaf:name":[{"@value":"Eko Siswanto"}],"jpcoar:affiliationName":[{"@value":"Hydrospheric Atmospheric Research Center Nagoya University  Nagoya Japan"},{"@value":"Agency for the Assessment and Application of Technology  Jakarta Indonesia"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943961681666","@type":"Researcher","foaf:name":[{"@value":"Joji Ishizaka"}],"jpcoar:affiliationName":[{"@value":"Faculty of Fisheries Nagasaki University  Nagasaki Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943961681665","@type":"Researcher","foaf:name":[{"@value":"Akihiko Morimoto"}],"jpcoar:affiliationName":[{"@value":"Hydrospheric Atmospheric Research Center Nagoya University  Nagoya Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943961681664","@type":"Researcher","foaf:name":[{"@value":"Katsuhisa Tanaka"}],"jpcoar:affiliationName":[{"@value":"Japan International Research Center for Agricultural Sciences  Tsukuba Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943961681537","@type":"Researcher","foaf:name":[{"@value":"Kazumaro Okamura"}],"jpcoar:affiliationName":[{"@value":"East China Sea Fisheries Oceanography Division Seikai National Fisheries Research Institute  Nagasaki Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943961681539","@type":"Researcher","foaf:name":[{"@value":"Agus Kristijono"}],"jpcoar:affiliationName":[{"@value":"Agency for the Assessment and Application of Technology  Jakarta Indonesia"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943961681538","@type":"Researcher","foaf:name":[{"@value":"Toshiro Saino"}],"jpcoar:affiliationName":[{"@value":"Hydrospheric Atmospheric Research Center Nagoya University  Nagoya Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2008-08","prism:volume":"35","prism:number":"15","prism:startingPage":"L15604"},"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%2F2008GL035040"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2008GL035040"}],"createdAt":"2008-08-11","modifiedAt":"2023-10-31","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001338209104384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Impact of cyclonic eddies and typhoons 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