{"created":"2023-07-25T11:02:05.848726+00:00","id":4260,"links":{},"metadata":{"_buckets":{"deposit":"350ae7f4-28f5-495a-8ae5-ece2646b6de5"},"_deposit":{"created_by":4,"id":"4260","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"4260"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00004260","sets":["1259:1260:1261:536:548"]},"author_link":["44148","44149","7781"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"Propagation of a quasi electrostatic whistler mode auroral hiss to the ground"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1998-12","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"29","bibliographicPageStart":"12","bibliographicVolumeNumber":"12","bibliographic_titles":[{"bibliographic_title":"Proceedings of the NIPR Symposium on Upper Atmosphere Physics"}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Matsuo,Toshio","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Nishiyama,Toshihiro","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Matsubara,Daisuke","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_1_description_1":{"attribute_name":"ページ属性","attribute_value_mlt":[{"subitem_description":"P(論文)","subitem_description_type":"Other"}]},"item_1_description_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"It has been thought from ray tracing studies that quasi electrostatic whistler mode auroral hiss is difficult to propagate down to the ground. To evaluate a refracting capability of VLF waves, we use the equations which were originally given by R. R. SCARABUCCI (1969). The refracting capability becomes gradually large with decreasing altitude in the height range above 2000km, and it becomes very large by a gradient of electron density below 2000km. It is confirmed from ray tracing and the calculation of the refracting capability that the wave normal of a quasi electrostatic whistler mode auroral hiss can enter the transmission cone at the ionospheric altitude when a latitudinally irregular magnetospheric plasma model is adopted, but, such a wave propagation is impossible with a simple diffusive equilibrium (DE) model. As the result, hiss is able to propagate down to the ground under the restricted condition.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00004260","subitem_identifier_reg_type":"JaLC"}]},"item_1_publisher_22":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"National Institute of Polar Research"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA10756224","subitem_source_identifier_type":"NCID"}]},"item_1_text_10":{"attribute_name":"著者所属(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Graduate School of Informatics, Kyoto University/Graduate School of Informatics, Kyoto University/Graduate School of Informatics, Kyoto University"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1998-12-01"}],"displaytype":"detail","filename":"KJ00000035963.pdf","filesize":[{"value":"2.4 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00000035963","url":"https://nipr.repo.nii.ac.jp/record/4260/files/KJ00000035963.pdf"},"version_id":"ffa37092-dd1d-4ce8-986a-29e5ceb1fb41"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"Propagation of a quasi electrostatic whistler mode auroral hiss to the ground","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Propagation of a quasi electrostatic whistler mode auroral hiss to the ground"}]},"item_type_id":"1","owner":"4","path":["548"],"pubdate":{"attribute_name":"公開日","attribute_value":"1998-12-01"},"publish_date":"1998-12-01","publish_status":"0","recid":"4260","relation_version_is_last":true,"title":["Propagation of a quasi electrostatic whistler mode auroral hiss to the ground"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T12:21:41.226875+00:00"}