{"@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/1360021391872615552.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2023jc019972"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2023JC019972"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Dual Wave Energy Sources for the Atlantic Niño Events Identified by Wave Energy Flux in Case Studies"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>The evolution of equatorial sea surface temperature anomalies during Atlantic Niño events has demonstrated its diversity in both intensity and timing. To investigate the mechanism responsible for this diversity, this study focuses on ocean responses to atmospheric forcing, manipulating the wind forcing in both equatorial and off‐equatorial regions to excite linear ocean models for three types of events that occurred in 1999, 2019, and 2021 respectively. The results reveal the dual wave energy sources for the equatorial Kelvin waves (KWs): one is the local wind forcing in the western tropical basin; the other is the reflection due to the off‐equatorial Rossby waves in the western boundary. The reflected KWs can precondition the events when wind‐forced KWs insufficiently displace the thermocline (e.g., the boreal winter of 2019 and 2021). The participation of off‐equatorial wave energy hence leads to the diversity of the Atlantic Niños.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380021391872615553","@type":"Researcher","foaf:name":[{"@value":"Qingyang Song"}],"jpcoar:affiliationName":[{"@value":"Key Laboratory of Marine Hazards Forecasting Ministry of Natural Resources Hohai University  Nanjing China"},{"@value":"College of Oceanography Hohai University  Nanjing China"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021391872615680","@type":"Researcher","foaf:name":[{"@value":"Youmin Tang"}],"jpcoar:affiliationName":[{"@value":"College of Oceanography Hohai University  Nanjing China"},{"@value":"Faculty of Environment University of Northern British Columbia  Prince George BC Canada"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021391872615552","@type":"Researcher","foaf:name":[{"@value":"Hidenori Aiki"}],"jpcoar:affiliationName":[{"@value":"Institute for Space‐Earth Environmental Research Nagoya University  Nagoya Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"21699275"},{"@type":"EISSN","@value":"21699291"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Oceans"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2023-07","prism:volume":"128","prism:number":"7","prism:startingPage":"e2023JC019972"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2023JC019972"}],"createdAt":"2023-06-30","modifiedAt":"2024-06-07","project":[{"@id":"https://cir.nii.ac.jp/crid/1040291932564661120","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"22H00176"},{"@type":"JGN","@value":"JP22H00176"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-22H00176/"}],"notation":[{"@language":"ja","@value":"大気と海洋の波動エネルギー循環のシームレス解析による熱帯・中緯度相互作用の解明"},{"@language":"en","@value":"Seamless Diagnosis of Atmospheric and Oceanic Wave Energy Circulation for Tropical and Mid-Latitude Interactions"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050300446003805440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Extraordinary Equatorial Atlantic Warming in Late 2019"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005518173537920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Climatological Horizontal Pattern of Energy Flux in the Tropical Atlantic as Identified by a Unified Diagnosis for Rossby and Kelvin Waves"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144324538112","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the connection between Benguela and equatorial Atlantic Niños and the role of the South Atlantic 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