{"@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/1892555065898753537.json","@type":"Researcher","foaf:Person":[{"foaf:name":[{"@value":"National Institute of Polar Research Tokyo (NiPR)"}]}],"product":[{"@id":"https://cir.nii.ac.jp/crid/1363670320109033472","@type":"Article","productIdentifier":[{"@type":"DOI","@value":"10.5194/angeo-19-205-2001"},{"@type":"URI","@value":"https://angeo.copernicus.org/articles/19/205/2001/angeo-19-205-2001.pdf"},{"@type":"HANDLE","@value":"2381/36581"}],"notation":[{"@value":"On the altitude dependence of the spectral characteristics of decametre-wavelength E region backscatter and the relationship with optical auroral forms"}],"relation":[{"type":"contributor"}]}],"dataSourceIdentifier":[{"@type":"OPENAIRE","@value":"doi_dedup___::76e1cbb59ad89d872e76eec1c939db9b_KgeduYziQSnYePw158yuHMGyExC_contributor"}]}