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雷放電の研究(第1報) : 雷放電の放電開始について
http://hdl.handle.net/2237/21747
http://hdl.handle.net/2237/217475cc99679-fc6c-465a-a947-ebcc70f0e205
名前 / ファイル | ライセンス | アクション |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2015-04-28 | |||||
タイトル | ||||||
タイトル | 雷放電の研究(第1報) : 雷放電の放電開始について | |||||
言語 | ja | |||||
その他のタイトル | ||||||
その他のタイトル | STUDIES OF THE LIGHTNING DISCHARGE Part 1. On the Initiation of Lightning Discharges | |||||
言語 | en | |||||
著者 |
石川, 晴治
× 石川, 晴治× 高木, 増美× 竹内, 利雄× ISIKAWA, Haruzi× TAKAGI, Masumi× TAKEUTI, Tosio |
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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 | Authors have investigated the initial portion of lightning discharges on the waveforms of atmospherics recorded with trigger method, and obtained following results: (1) More than 80 % of lightning discharges occurring within the range 150 km. are cloud discharges. (2) The initial portion of the stepped leader of a ground discharge must be cloud discharges producing very similar waveforms to the true α type stepped leader. (3) Some of the stepped leaders have no initial pulses, and the leader begins with a group of isolated pulses or with high frequency pulsations, which seems to mean that the leader begins without any leading cloud discharges described in paragraph(2). The situation is also the same for the case of cloud discharges. | |||||
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 8, 号 1-2, p. 1-10, 発行日 1958-03-20 |
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著者版フラグ | ||||||
値 | publisher | |||||
URI | ||||||
識別子 | http://hdl.handle.net/2237/21747 | |||||
識別子タイプ | HDL |