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Relationship between ionospheric conductivity and intensity of the daytime region 1 field-aligned current in geomagnetically quiet conditions
https://iwate-u.repo.nii.ac.jp/records/12632
https://iwate-u.repo.nii.ac.jp/records/126321ccab39d-fff1-4a2f-aae2-771e3b5d814b
名前 / ファイル | ライセンス | アクション |
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jgr-v108na5p1190-1197.pdf (496.3 kB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2013-01-07 | |||||
タイトル | ||||||
タイトル | Relationship between ionospheric conductivity and intensity of the daytime region 1 field-aligned current in geomagnetically quiet conditions | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | region 1 field-aligned current | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | ionospheric conductivity | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | current generator | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | voltage generator | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | low-latitude boundary layer | |||||
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 | journal article | |||||
著者 |
Yamamoto, T
× Yamamoto, T× Ozaki, M× Inoue, S |
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著者(機関) | ||||||
値 | Department of Earth and Planetary Science, University of Tokyo | |||||
著者(機関) | ||||||
値 | Institute of Industrial Science, University of Tokyo | |||||
著者(機関) | ||||||
値 | Faculty of Education, Iwate University | |||||
登録日 | ||||||
日付 | 2013-01-07 | |||||
書誌情報 |
Journal of Geophysical Research Space Physics 巻 108, 号 A5, p. 1190-1197, 発行日 2003-05-01 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0148-0227 | |||||
Abstract | ||||||
内容記述タイプ | Other | |||||
内容記述 | The relationship between the region 1 field-aligned current (FAC) intensity and the ionospheric conductivity in geomagnetically quiet conditions has been believed to be useful to determine whether the FAC is driven by a voltage generator or a current generator. This paper, however, shows that at least for daytime (0800–1600 MLT) FACs, the current generator has the same characteristic of “linear relationship between the current intensity and the conductivity” as the voltage generator. This conclusion is obtained due to the fact that the sum of Pedersen conductivities, maintained by solar EUV ionization, at two conjugate points on the northern and southern ionospheres is approximately independent of the solar zenith angle at either of these points. Notably, the pressure-gradient-driven model for the generation of the region 1 FAC from the low-latitude boundary layer is then consistent with observations that the current intensity increases linearly with the height-integrated Pedersen conductivity. | |||||
出版者 | ||||||
出版者 | American Geophysical Union | |||||
権利 | ||||||
権利情報 | © 2003 American Geophysical Union | |||||
DOI | ||||||
関連タイプ | isIdenticalTo | |||||
識別子タイプ | DOI | |||||
関連識別子 | 10.1029/2002JA009607 | |||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |