{"@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/1363670320687536640.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/158668a0"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/158668a0.pdf"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/158668a0"}}],"dc:title":[{"@value":"Geomagnetic Control of Region F2 of the Ionosphere"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380285711828918916","@type":"Researcher","foaf:name":[{"@value":"S. K. MITRA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00280836"},{"@type":"EISSN","@value":"14764687"}],"prism:publicationName":[{"@value":"Nature"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"1946-11","prism:volume":"158","prism:number":"4019","prism:startingPage":"668","prism:endingPage":"669"},"reviewed":"false","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://www.nature.com/articles/158668a0.pdf"},{"@id":"http://www.nature.com/articles/158668a0"}],"createdAt":"2008-01-03","modifiedAt":"2021-12-01","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050564285769724160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Temporal change of EIA asymmetry revealed by a beacon receiver network in Southeast Asia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708261620224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Super plasma fountain and equatorial ionization anomaly during penetration electric field"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584339750694656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Responses of the African-European equatorial-, low-, mid-, and high-latitude ionosphere to geomagnetic storms of 2013, 2015 St Patrick’s Days, 1 June 2013, and 7 October 2015"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1038/158668a0"},{"@type":"CROSSREF","@value":"10.1029/2008ja013768_references_DOI_3WzK5G3JVnInMd4SyH8PegzyjBa"},{"@type":"CROSSREF","@value":"10.1186/s40623-015-0252-9_references_DOI_3WzK5G3JVnInMd4SyH8PegzyjBa"},{"@type":"CROSSREF","@value":"10.1016/j.asr.2022.10.029_references_DOI_3WzK5G3JVnInMd4SyH8PegzyjBa"}]}