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LIDAR OBSERVATIONS OF THE MESOSPHERIC SODIUM LAYER AT SYOWA STATION, ANTARCTICA
https://doi.org/10.15094/00003539
https://doi.org/10.15094/000035392cc56978-041f-4c51-b60a-137bfd4aa8f4
名前 / ファイル | ライセンス | アクション |
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KJ00000767747 (82.7 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1987-09-01 | |||||
タイトル | ||||||
タイトル | LIDAR OBSERVATIONS OF THE MESOSPHERIC SODIUM LAYER AT SYOWA STATION, ANTARCTICA | |||||
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 | |||||
ID登録 | ||||||
ID登録 | 10.15094/00003539 | |||||
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) | |||||
記事種別(英) | ||||||
en | ||||||
ABSTRACT | ||||||
論文名よみ | ||||||
その他のタイトル | LIDAR OBSERVATIONS OF THE MESOSPHERIC SODIUM LAYER AT SYOWA STATION, ANTARCTICA | |||||
著者名よみ |
ノムラ, アキオ
× ノムラ, アキオ× イワサカ, ヤスノブ× フクニシ, ヒロシ× ヒラサワ, タケオ× カワグチ, サダオ× カノ, テツオ |
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著者名(英) |
NOMURA, Akio
× NOMURA, Akio× IWASAKA, Yasunobu× FUKUNISHI, Hiroshi× HIRASAWA, Takeo× KAWAGUCHI, Sadao× KANO, Tetsuo |
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著者所属(英) | ||||||
en | ||||||
Faculty of Engineering, Shinshu University | ||||||
著者所属(英) | ||||||
en | ||||||
Water Research Institute, Nagoya University | ||||||
著者所属(英) | ||||||
en | ||||||
Upper Atmosphere and Space Research Laboratory, Tohoku University | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
著者所属(英) | ||||||
en | ||||||
Faculty of Engineering, Shinshu University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The mesospheric sodium layer has been measured on 42 nights during the period from April to October 1985 at Syowa Station (69°00′E, 39°35′E), Antarctica, by observation of the resonance scattering of a tuned dye laser beam, which has been made as part of the Middle Atmosphere Program (MAP). There are no pronounced seasonal variations in abundance, the peak height and the width of the sodium layer. No enhancement of aboundance in winter has been observed, which is different from those obtained at mid-latitudes in the northern hemisphere. It is, however, interesting to show the oscillatory variation in abundance with a period of about 40 days. The nocturnal variations of sodium profile show wave-like structure with a vertical wavelength of 10 to 16km and a period of 4 to 8h, which suggests the existence of gravity wave. During sodium lidar measurements under auroral activity, it has been observed by chance that the layer is disturbed by auroral break-up associated with the change of cosmic noise absorption (CNA). | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA10756213 | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 巻 1, p. 150, 発行日 1987-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |