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Characteristics of subionospheric VLF perturbations associated with winter lightning around Japan
https://doi.org/10.15094/00006382
https://doi.org/10.15094/00006382f7d4c696-b8d2-4c4e-98e8-9d96dedd58fb
名前 / ファイル | ライセンス | アクション |
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KJ00000729604 (550.3 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 2004-08-01 | |||||
タイトル | ||||||
タイトル | Characteristics of subionospheric VLF perturbations associated with winter lightning around Japan | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Trimpis | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | VLF subionospheric propagation | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | winter lightning | |||||
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 | |||||
ID登録 | ||||||
ID登録 | 10.15094/00006382 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Otsuyama, Takuya
× Otsuyama, Takuya× Manabe, Jun× Hayakawa, Masashi |
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著者所属(英) | ||||||
en | ||||||
Department of Electronic Engineering, The University of Electro-Communications | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Electronic Engineering, The University of Electro-Communications | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Electronic Engineering, The University of Electro-Communications | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | VLF signature of ionospheric perturbations associated with winter lightning discharges around Japan has been investigated during 3 months observation (December 2000 through February 2001). During this period it seems that there are no optical phenomena in the Hokuriku area (Sea of Japan side) indicating that our period was not extremely active in lightning as compared with the previous winter (Y. Hobara et al., Geophys. Res. Lett., 28, 935, 2001). Based on the VLF subionospheric observation at Moshiri (Hokkaido) and Maizuru (near Kyoto) for NWC (Australia) and NPM (Hawaii) transmitter signals, we have found the following results; (1) Trimpis tend to occur at least when the lightning activity is enhanced independent of the polarity, (2) Trimpis are observed when the causative lightning is located not only on the Sea of Japan side but also on the Pacific Ocean side, and (3) the occurrence of Trimpis in the Hokuriku area is more enhanced than that on the Pacific side, which is discussed with a special reference to the different meteorological conditions. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA11397422 | |||||
書誌情報 |
Advances in polar upper atmosphere research 巻 18, p. 77-86, 発行日 2004-08 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |