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ON THE NATURE OF FREQUENCY SPECTRUM OF ATMOSPHERIC SOURCE SIGNALS
http://hdl.handle.net/2237/21909
http://hdl.handle.net/2237/21909ab8b84f4-1b18-4eea-aaaa-29b833cc01ad
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
proria_14_1.pdf (877.8 kB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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| 公開日 | 2015-05-15 | |||||
| タイトル | ||||||
| タイトル | ON THE NATURE OF FREQUENCY SPECTRUM OF ATMOSPHERIC SOURCE SIGNALS | |||||
| 言語 | en | |||||
| 著者 |
IWATA, Akira
× IWATA, Akira× KANADA, Masahiro |
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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 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | The peak intensity spectra of atmospheric source signals have been investigated in a high frequency range to see the influence of different processes involved in lightning discharge on the nature of an intensity spectrum. It has been shown that a return stroke is the strongest source of an atmospheric source signal below a few Mc/s, while it tends to be a weaker source as the frequency is increased beyond 15 Mc/s. The recoil process which is responsible for a K-change becomes predominant beyond several Mc/s. It has been found that the break-down process preceding a leader process is not predominant in the frequency range investigated. | |||||
| 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 | ||||||
| 資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
| 資源タイプ | 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 14, p. 1-6, 発行日 1967-03-20 |
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| 著者版フラグ | ||||||
| 値 | publisher | |||||
| URI | ||||||
| 識別子 | http://hdl.handle.net/2237/21909 | |||||
| 識別子タイプ | HDL | |||||
