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<論文>夜間大気光0_2 Atmospheric及びOHマイネル帯のロケット観測
https://jaxa.repo.nii.ac.jp/records/32493
https://jaxa.repo.nii.ac.jp/records/324934c212ce6-18a6-4d67-a838-73eeb7539889
名前 / ファイル | ライセンス | アクション |
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SA0125776.pdf (878.5 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2015-03-26 | |||||
タイトル | ||||||
タイトル | <論文>夜間大気光0_2 Atmospheric及びOHマイネル帯のロケット観測 | |||||
言語 | ||||||
言語 | jpn | |||||
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 | |||||
その他のタイトル(英) | ||||||
その他のタイトル | Rocket measurements of 0_2 Atmospheric and OH Meinel Bands in the Nightglow | |||||
著者 |
渡辺, 隆
× 渡辺, 隆× 中村, 正年× 小川, 利紘× WATANABE, Takashi× NAKAMURA, Masatoshi× OGAWA, Toshihiro |
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著者所属 | ||||||
筑波大学物理学系 | ||||||
著者所属 | ||||||
筑波大学物理学系 | ||||||
著者所属 | ||||||
東京大学理学部 | ||||||
出版者 | ||||||
出版者 | 東京大学宇宙航空研究所 | |||||
書誌情報 |
東京大学宇宙航空研究所報告 巻 15, 号 3_B, p. 509-524, 発行日 1979-10 |
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抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Altitude distributions of the (0,0) 7619A band of O_2 atmospheric system (b^1Σ^+_g-X^3Σ^-_g) and of the (7,2) 6863A band of OH (X^2Π) in the night airglow emissions were measured at 31°N latitude. In spite of different seasons and local times of observations, all three measurements presented the peak emission rate occuring at an altitude of 94 ± 1 km for the O_2 band and at 90 ± 2 km for the OH band. The former emitting altitude is in basic agreement with the atomic oxygen density profile measured by the UV resonance fluorescence method, but the latter is considerably higher than expected from relevant theoretical models. After examining various possible causes for this discrepance, it is possible that the continuum airglow may contaminate our observations of the OH airglow. This may be aplicable also to other similar observations made so far in the near infrared. | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0563-8100 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00161914 | |||||
資料番号 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 資料番号: SA0125776000 |