WEKO3
アイテム
SOME RESULTS OF THE WAVE FORM OF ATMOSPHERICS
http://hdl.handle.net/2237/21471
http://hdl.handle.net/2237/214718407bcc2-3300-4f28-aede-6eeb44e969bf
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
Vol2-3.pdf (851.1 kB)
|
|
| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2015-04-07 | |||||
| タイトル | ||||||
| タイトル | SOME RESULTS OF THE WAVE FORM OF ATMOSPHERICS | |||||
| 言語 | en | |||||
| 著者 |
SAO, KAZUO
× 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 | ||||||
| 内容記述タイプ | Abstract | |||||
| 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 | |||||
| 出版者 | ||||||
| 出版者 | The Research Institute of Atmospherics, Nagoya University | |||||
| 言語 | en | |||||
| 言語 | ||||||
| 言語 | eng | |||||
| 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 | 0077-264X | |||||
| 書誌情報 |
en : Proceedings of the Research Institute of Atmospherics, Nagoya University 巻 2, p. 26-30, 発行日 1954-03-30 |
|||||
| 著者版フラグ | ||||||
| 値 | publisher | |||||
| URI | ||||||
| 識別子 | http://hdl.handle.net/2237/21471 | |||||
| 識別子タイプ | HDL | |||||
