{"@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/1390282681490218112.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1186/bf03351804"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"7285412"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/7285412"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I7285412"}},{"identifier":{"@type":"URI","@value":"https://dl.ndl.go.jp/pid/8943476"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/content/pdf/10.1186/BF03351804.pdf"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/article/10.1186/BF03351804/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1186/BF03351804"}},{"identifier":{"@type":"NAID","@value":"10017467621"}},{"identifier":{"@type":"NAID","@value":"130003781063"}}],"dc:title":[{"@language":"en","@value":"A 3-D current system of an ionospheric dynamo including a skin effect in an anisotropic plasma"},{"@language":"ja-Kana","@value":"3 D current system of an ionospheric dynamo including a skin effect in an anisotropic plasma"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"The numerical two-mode electromagnetic model of an ionospheric dynamo is constructed taking into account a skin effect of a field in an anisotropic plasma, i.e. a non-potential electric field of Sq-variations in the ionosphere. It is shown that a three-dimensional current system generated by the dynamo action of winds is located at altitudes less than about 200 km basically. It does not depend on an ionosphere condition in upper layers and weaker field-aligned currents between the northern and southern hemispheres practically, and an almost complete closed current circuit is generated in the dynamo layer."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410282681490218112","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000001756030"},{"@type":"NRID","@value":"9000254263077"}],"foaf:name":[{"@language":"en","@value":"Plotkin V. V."}],"jpcoar:affiliationName":[{"@language":"en","@value":"Institute of geophysics SB RAS"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"13438832"},{"@type":"EISSN","@value":"18805981"},{"@type":"NDL_BIB_ID","@value":"000000159136"},{"@type":"ISSN","@value":"13438832"},{"@type":"LISSN","@value":"13438832"},{"@type":"NCID","@value":"AA11211921"}],"prism:publicationName":[{"@language":"en","@value":"Earth, Planets and Space"},{"@language":"ja","@value":"Ｅａｒｔｈ，　Ｐｌａｎｅｔｓ　ａｎｄ　Ｓｐａｃｅ"},{"@language":"en","@value":"Earth Planets Space"},{"@language":"ja","@value":"Ｅａｒｔｈ　Ｐｌａｎｅｔｓ　Ｓｐａｃｅ"}],"dc:publisher":[{"@language":"en","@value":"Society of Geomagnetism and Earth, Planetary and Space Sciences, The Seismological Society of Japan, The Volcanological Society of Japan , The Geodetic Society of Japan , The Japanese Society for Planetary Sciences"},{"@language":"ja","@value":"地球電磁気・地球惑星圏学会 、公益社団法人 日本地震学会、特定非営利活動法人 日本火山学会、日本測地学会、日本惑星科学会"}],"prism:publicationDate":"2005","prism:volume":"57","prism:number":"1","prism:startingPage":"35","prism:endingPage":"45"},"reviewed":"false","url":[{"@id":"http://id.ndl.go.jp/bib/7285412"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I7285412"},{"@id":"https://dl.ndl.go.jp/pid/8943476"},{"@id":"https://link.springer.com/content/pdf/10.1186/BF03351804.pdf"},{"@id":"https://link.springer.com/article/10.1186/BF03351804/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1186/BF03351804"}],"availableAt":"2005","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Ionospheric%20dynamo","dc:title":"Ionospheric dynamo"},{"@id":"https://cir.nii.ac.jp/all?q=skin%20effect","dc:title":"skin effect"},{"@id":"https://cir.nii.ac.jp/all?q=non-potential%20electric%20field","dc:title":"non-potential electric field"},{"@id":"https://cir.nii.ac.jp/all?q=Sq-variation","dc:title":"Sq-variation"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011144408613248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Electrodynamic effects of thermospheric winds from the NCAR Thermospheric General Circulation Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095915380224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geoelectromagnetic Investigation of the Earth’s Crust and Mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569859318144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A numerical model of the ionospheric dynamo—I. 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