WEKO3
アイテム
空電波形に関する2,3の結果
http://hdl.handle.net/2237/21641
http://hdl.handle.net/2237/21641391b33ef-a777-48c8-92c9-2a12c4aa016f
名前 / ファイル | ライセンス | アクション |
---|---|---|
bulria_4_2_86.pdf (644.9 kB)
|
|
Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 2015-04-21 | |||||
タイトル | ||||||
タイトル | 空電波形に関する2,3の結果 | |||||
言語 | ja | |||||
その他のタイトル | ||||||
その他のタイトル | SOME RESULTS OF WAVE FORM OF ATMOSPHERICS | |||||
言語 | en | |||||
著者 |
佐尾, 和夫
× 佐尾, 和夫× 仲井, 猛敏× SAO, Kazuo× NAKAI, Taketoshi |
|||||
アクセス権 | ||||||
アクセス権 | open access | |||||
アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||
抄録 | ||||||
内容記述 | The observations of atmospherics were made in September 1952 and in September 1953. The wave forms were recorded and the fixing of sources was conducted by triangulation at Toyokawa, Akita and Kumamoto. Waveforms of the regular peaked type at night were analysed on the reflection theory, and the reflection height of the ionosphere and the distance of the source were calculated. Several waveforms from the same sources received at Toyokawa and Akita were discussed. Some examples were shown, indicating that the quasi-period of the second half cycle of the oscillatory component increases with distance, and its rough explanation was given. | |||||
言語 | en | |||||
内容記述タイプ | Abstract | |||||
出版者 | ||||||
言語 | ja | |||||
出版者 | 名古屋大学空電研究所 | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
出版タイプ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
ISSN(print) | ||||||
収録物識別子タイプ | PISSN | |||||
収録物識別子 | 0465-7756 | |||||
書誌情報 |
ja : 空電研究所報告 巻 4, 号 2, p. 86-89, 発行日 1954-03-30 |
|||||
著者版フラグ | ||||||
値 | publisher | |||||
URI | ||||||
識別子 | http://hdl.handle.net/2237/21641 | |||||
識別子タイプ | HDL |