{"@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/1360565166758027776.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/ncomms9268"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/ncomms9268.pdf"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/ncomms9268"}},{"identifier":{"@type":"PMID","@value":"26369503"}},{"identifier":{"@type":"HANDLE","@value":"1956/11752"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Solar forcing synchronizes decadal North Atlantic climate variability"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Quasi-decadal variability in solar irradiance has been suggested to exert a substantial effect on Earth’s regional climate. In the North Atlantic sector, the 11-year solar signal has been proposed to project onto a pattern resembling the North Atlantic Oscillation (NAO), with a lag of a few years due to ocean-atmosphere interactions. The solar/NAO relationship is, however, highly misrepresented in climate model simulations with realistic observed forcings. In addition, its detection is particularly complicated since NAO quasi-decadal fluctuations can be intrinsically generated by the coupled ocean-atmosphere system. Here we compare two multi-decadal ocean-atmosphere chemistry-climate simulations with and without solar forcing variability. While the experiment including solar variability simulates a 1–2-year lagged solar/NAO relationship, comparison of both experiments suggests that the 11-year solar cycle synchronizes quasi-decadal NAO variability intrinsic to the model. The synchronization is consistent with the downward propagation of the solar signal from the stratosphere to the surface.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380847869924837888","@type":"Researcher","foaf:name":[{"@value":"Rémi Thiéblemont"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869924837889","@type":"Researcher","foaf:name":[{"@value":"Katja Matthes"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869924837891","@type":"Researcher","foaf:name":[{"@value":"Nour-Eddine Omrani"}]},{"@id":"https://cir.nii.ac.jp/crid/1030003658481498114","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"70343887"},{"@type":"NRID","@value":"1000070343887"},{"@type":"NRID","@value":"9000363497438"},{"@type":"NRID","@value":"9000363503773"},{"@type":"NRID","@value":"9000240186417"},{"@type":"NRID","@value":"9000257827832"},{"@type":"NRID","@value":"9000237869566"},{"@type":"NRID","@value":"9000283228245"},{"@type":"NRID","@value":"9000288831592"},{"@type":"NRID","@value":"9000311489029"},{"@type":"NRID","@value":"9000363503778"},{"@type":"NRID","@value":"9000240187145"},{"@type":"NRID","@value":"9000391736180"},{"@type":"NRID","@value":"9000350622936"},{"@type":"NRID","@value":"9000252948261"},{"@type":"NRID","@value":"9000392814777"},{"@type":"NRID","@value":"9000251014357"},{"@type":"NRID","@value":"9000003402752"},{"@type":"NRID","@value":"9000288830747"},{"@type":"NRID","@value":"9000311489490"},{"@type":"NRID","@value":"9000345224809"},{"@type":"NRID","@value":"9000363492786"},{"@type":"NRID","@value":"9000239868192"},{"@type":"NRID","@value":"9000347546984"},{"@type":"NRID","@value":"9000392819294"},{"@type":"NRID","@value":"9000007403340"},{"@type":"NRID","@value":"9000270295224"},{"@type":"NRID","@value":"9000311489329"},{"@type":"NRID","@value":"9000362241069"},{"@type":"NRID","@value":"9000392818714"},{"@type":"NRID","@value":"9000392817364"},{"@type":"NRID","@value":"9000283236643"},{"@type":"NRID","@value":"9000240186382"},{"@type":"NRID","@value":"9000392819329"},{"@type":"NRID","@value":"9000392818761"},{"@type":"NRID","@value":"9000283228257"},{"@type":"NRID","@value":"9000283593644"},{"@type":"NRID","@value":"9000363500183"},{"@type":"NRID","@value":"9000270295328"},{"@type":"NRID","@value":"9000317129757"},{"@type":"NRID","@value":"9000392815763"},{"@type":"NRID","@value":"9000375915264"},{"@type":"NRID","@value":"9000237754051"},{"@type":"NRID","@value":"9000257766661"},{"@type":"NRID","@value":"9000257827961"},{"@type":"NRID","@value":"9000288831262"},{"@type":"NRID","@value":"9000311488244"},{"@type":"NRID","@value":"9000283228414"},{"@type":"NRID","@value":"9000270295312"},{"@type":"NRID","@value":"9000283700374"},{"@type":"NRID","@value":"9000009164360"},{"@type":"NRID","@value":"9000363488462"},{"@type":"NRID","@value":"9000257979005"},{"@type":"NRID","@value":"9000237869564"},{"@type":"NRID","@value":"9000401587119"},{"@type":"NRID","@value":"9000283236619"},{"@type":"NRID","@value":"9000010448504"},{"@type":"NRID","@value":"9000363497416"},{"@type":"NRID","@value":"9000363484942"},{"@type":"NRID","@value":"9000363498121"},{"@type":"NRID","@value":"9000363498057"}],"foaf:name":[{"@value":"Kunihiko Kodera"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869924837890","@type":"Researcher","foaf:name":[{"@value":"Felicitas Hansen"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"20411723"}],"prism:publicationName":[{"@value":"Nature Communications"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2015-09-15","prism:volume":"6","prism:number":"1","prism:startingPage":"8268"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://creativecommons.org/licenses/by/4.0","https://creativecommons.org/licenses/by/4.0"],"url":[{"@id":"https://www.nature.com/articles/ncomms9268.pdf"},{"@id":"https://www.nature.com/articles/ncomms9268"}],"createdAt":"2015-09-15","modifiedAt":"2023-01-05","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=VDP::Matematikk%20og%20Naturvitenskap:%20400","dc:title":"VDP::Matematikk og Naturvitenskap: 400"},{"@id":"https://cir.nii.ac.jp/all?q=551","dc:title":"551"},{"@id":"https://cir.nii.ac.jp/all?q=Article","dc:title":"Article"},{"@id":"https://cir.nii.ac.jp/all?q=Earth%20sciences","dc:title":"Earth sciences"},{"@id":"https://cir.nii.ac.jp/all?q=Climate%20science","dc:title":"Climate science"},{"@id":"https://cir.nii.ac.jp/all?q=Atmospheric%20science","dc:title":"Atmospheric science"},{"@id":"https://cir.nii.ac.jp/all?q=:Matematikk%20og%20Naturvitenskap:%20400%20%5BVDP%5D","dc:title":":Matematikk og Naturvitenskap: 400 [VDP]"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782191722880","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"24224011"},{"@type":"JGN","@value":"JP24224011"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-24224011/"}],"notation":[{"@language":"ja","@value":"成層圏‐対流圏結合系における極端気象変動の現在・過去・未来"},{"@language":"en","@value":"Extreme Weather Variations in the Stratosphere -Troposphere Coupled"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257260381952","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26281016"},{"@type":"JGN","@value":"JP26281016"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26281016/"}],"notation":[{"@language":"ja","@value":"太陽活動の北極振動への影響とメカニズムの解明"},{"@language":"en","@value":"Elucidation of effect and mechanism of solar activity on the Arctic Oscillation"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011144808093056","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Annular mode changes in the CMIP5 simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146048873472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Recent variability of the solar spectral irradiance and its impact on climate modelling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282427406208","@type":"Article","resourceType":"学術雑誌論文(journal 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Oscillation"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469916418944","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A possible mechanism of solar modulation of the spatial structure of the North Atlantic Oscillation"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943559295104","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modeling the Sun’s Magnetic Field and Irradiance since 1713"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944575837056","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Northern hemisphere winter climate response to greenhouse gas, ozone, solar, and volcanic forcing"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544418290067968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The North Atlantic 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