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SEA EFFECT DUE TO THE HIGH ALTITUDE NUCLEAR EXPLOSION
http://hdl.handle.net/2237/21870
http://hdl.handle.net/2237/21870c400cea9-f3e1-4e74-bc4f-8731a5b42a06
名前 / ファイル | ライセンス | アクション |
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proria_12_19.pdf (931.6 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2015-05-12 | |||||
タイトル | ||||||
タイトル | SEA EFFECT DUE TO THE HIGH ALTITUDE NUCLEAR EXPLOSION | |||||
言語 | en | |||||
著者 |
KAMADA, Tetsuo
× KAMADA, Tetsuo |
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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 | Sudden abnormal changes of VLF atmospherics intensities, caused by the very high altitude nuclear explosion over Johnston Island on July 9th 1962, were observed at Toyokawa, Japan. The aspect of this anomalies on records was just the same as SEA caused by solar flares. On the occasion, as the sun was quiet and the onset of the anomalies coincided with the explosion, it seems to me that the anomalies were caused by bomb-induced ionization in the ionospheric D layer. So, it was named "the SEA effect due to nuclear explosion". In this paper are reported the observation results and a comment on the order of disturbances in the ionospheric D layer. | |||||
言語 | en | |||||
内容記述タイプ | Abstract | |||||
出版者 | ||||||
言語 | en | |||||
出版者 | The Research Institute of Atmospherics, Nagoya University | |||||
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 12, p. 19-25, 発行日 1965-03-25 |
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著者版フラグ | ||||||
値 | publisher | |||||
URI | ||||||
識別子 | http://hdl.handle.net/2237/21870 | |||||
識別子タイプ | HDL |