{"created":"2023-05-15T16:44:44.697974+00:00","id":20517,"links":{},"metadata":{"_buckets":{"deposit":"3cb45030-6016-4c4e-87f4-b67d7c608399"},"_deposit":{"created_by":2,"id":"20517","owners":[2],"pid":{"revision_id":0,"type":"depid","value":"20517"},"status":"published"},"_oai":{"id":"oai:nagasaki-u.repo.nii.ac.jp:00020517","sets":["1273:1274:1408:1420"]},"author_link":["86632","86631"],"item_3_alternative_title_19":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"The wind system and the temperature variation in the case of heating the lower part of the Thermosphere periodically"}]},"item_3_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1971-12-25","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"13","bibliographicPageStart":"7","bibliographicVolumeNumber":"12","bibliographic_titles":[{"bibliographic_title":"長崎大学教養部紀要. 自然科学"}]}]},"item_3_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"A wind system and pressure and temperature oscillations are studied when the lower part of the Thermosphere (around 90-110 km) is heated periodically. The obtained results are follows: (1) the wind components and all oscillations predominate in and above the heating layer, (2) only one node is formed in the heating layer in the case of the westerly, northerly and pressure oscillation, and therefore, these phases have a jump of 180 in the same layer, (3) in the case of the vertical wind and the temperature oscillation, no node is formed.","subitem_description_type":"Abstract"}]},"item_3_description_64":{"attribute_name":"引用","attribute_value_mlt":[{"subitem_description":"長崎大学教養部紀要. 自然科学. 1971, 12, p.7-13","subitem_description_type":"Other"}]},"item_3_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"86632","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Matsushima, A."}]}]},"item_3_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN00178360","subitem_source_identifier_type":"NCID"}]},"item_3_source_id_7":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"02871319","subitem_source_identifier_type":"ISSN"}]},"item_3_text_62":{"attribute_name":"sortkey","attribute_value_mlt":[{"subitem_text_value":"P00007-P00013"}]},"item_3_version_type_16":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"松島, 晟"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2020-12-23"}],"displaytype":"detail","filename":"kyoyoS12_00_02_t.pdf","filesize":[{"value":"373.6 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"kyoyoS12_00_02_t.pdf","url":"https://nagasaki-u.repo.nii.ac.jp/record/20517/files/kyoyoS12_00_02_t.pdf"},"version_id":"f41f500f-ff1e-4da7-80e1-1e9b0d9d2e3c"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"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":"熱圏下部を周期的に加熱した場合の風系と温度変化について","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"熱圏下部を周期的に加熱した場合の風系と温度変化について"}]},"item_type_id":"3","owner":"2","path":["1420"],"pubdate":{"attribute_name":"公開日","attribute_value":"2008-04-11"},"publish_date":"2008-04-11","publish_status":"0","recid":"20517","relation_version_is_last":true,"title":["熱圏下部を周期的に加熱した場合の風系と温度変化について"],"weko_creator_id":"2","weko_shared_id":-1},"updated":"2023-05-16T02:32:40.525631+00:00"}