{"@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/1361699996161107968.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/1999gl900507"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F1999GL900507"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/1999GL900507"}},{"identifier":{"@type":"NAID","@value":"30013362793"}}],"dc:title":[{"@value":"Role of planetary waves in the stratosphere‐troposphere coupled variability in the northern hemisphere winter"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The role of planetary waves in stratosphere‐troposphere coupled variability is investigated using an extended singular value decomposition analysis of zonal‐mean zonal wind and the vertical component of the Eliassen‐Palm (E‐P) flux for the winters from 1979/80 to 1995/96. The results suggest a close relationship between anomalies of zonal‐mean zonal wind and the convergence zone of E‐P flux, which together shift poleward and downward from the stratosphere to the troposphere as time advances. Following enhanced vertical propagation of waves into the stratosphere, the Arctic Oscillation (AO) pattern is seen in the 500 hPa geopotential height field in association with an increased poleward propagation of tropospheric waves.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699996161107968","@type":"Researcher","foaf:name":[{"@value":"Yuhji Kuroda"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699996161107969","@type":"Researcher","foaf:name":[{"@value":"Kunihiko Kodera"}]}],"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":"1999-08","prism:volume":"26","prism:number":"15","prism:startingPage":"2375","prism:endingPage":"2378"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F1999GL900507"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/1999GL900507"}],"createdAt":"2003-12-08","modifiedAt":"2023-11-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050017057728463104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stratospheric tropical warming event and its impact on the polar and tropical troposphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1050306506453255168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"成層圏対流圏結合"},{"@language":"en","@value":"Stratosphere-troposhere coupling"},{"@value":"[日本気象学会]創立125周年記念解説 成層圏対流圏結合"},{"@language":"ja-Kana","@value":"ニホン キショウ ガッカイ ソウリツ 125シュウネン キネン カイセツ セイソウケン タイリュウケン ケツゴウ"},{"@value":"成層圏対流圏結合(創立125周年記念解説)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004230284709504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The predictability of the extratropical stratosphere on monthly time‐scales and its impact on the skill of tropospheric forecasts"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567190136224896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"How can we understand the global distribution of the solar cycle signal on\nthe Earth's surface?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641637194752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tropospheric impact of reflected planetary waves from the stratosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641637204864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Role of the stratosphere on the predictability of medium‐range weather forecast: A case study of winter 2003–2004"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204229788800","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Climate Variations from the Viewpoint of the Arctic"},{"@language":"ja","@value":"北極圏からみた気候変動"},{"@language":"ja-Kana","@value":"ホッキョクケン カラ ミタ キコウ ヘンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205223194112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Delayed North Atlantic Response to Solar Forcing of the Stratospheric Polar Vortex"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206501404416","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Interannual Seesaw between the Aleutian and Icelandic Lows. 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