{"@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/1361137046437653376.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.dsr.2004.06.005"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0967063704001141?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0967063704001141?httpAccept=text/plain"}}],"dc:title":[{"@value":"The Rossby wave as a key mechanism of Indian Ocean climate variability"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137046437653376","@type":"Researcher","foaf:name":[{"@value":"Mark R. Jury"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137046437653377","@type":"Researcher","foaf:name":[{"@value":"Bohua Huang"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"09670637"}],"prism:publicationName":[{"@value":"Deep Sea Research Part I: Oceanographic Research Papers"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2004-12","prism:volume":"51","prism:number":"12","prism:startingPage":"2123","prism:endingPage":"2136"},"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:S0967063704001141?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0967063704001141?httpAccept=text/plain"}],"createdAt":"2004-10-13","modifiedAt":"2025-10-18","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050566774745486720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Life Cycle of Annual Waves in the Indian Ocean as Identified by Seamless Diagnosis of the Energy Flux"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617497708160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Enhanced Meiyu‐Baiu Rainfall in Early Summer 2020: Aftermath of the 2019 Super IOD Event"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302864774683776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Decadal modulation of ENSO and IOD impacts on the Indian Ocean upwelling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360864734597338368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The influence of tropical and subtropical modes of climate variability on precipitation in Mozambique"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266988436736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The vertical structure of annual wave energy flux in the tropical Indian Ocean"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.dsr.2004.06.005"},{"@type":"CROSSREF","@value":"10.1029/2020gl090671_references_DOI_NMeDacTh2CEnZ1YvHJ4Wa9rAbJS"},{"@type":"CROSSREF","@value":"10.3389/feart.2023.1212421_references_DOI_NMeDacTh2CEnZ1YvHJ4Wa9rAbJS"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00432-9_references_DOI_NMeDacTh2CEnZ1YvHJ4Wa9rAbJS"},{"@type":"CROSSREF","@value":"10.1002/joc.8509_references_DOI_NMeDacTh2CEnZ1YvHJ4Wa9rAbJS"},{"@type":"CROSSREF","@value":"10.1029/2019gl085670_references_DOI_NMeDacTh2CEnZ1YvHJ4Wa9rAbJS"}]}