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Upper stratospheric temperature profiles obtained by lidar at Syowa Station, Antarctica
https://doi.org/10.15094/00003558
https://doi.org/10.15094/0000355891a3c37b-b58a-47b8-ae58-62c04db8fed7
名前 / ファイル | ライセンス | アクション |
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KJ00000035524 (1.0 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1989-08-01 | |||||
タイトル | ||||||
タイトル | Upper stratospheric temperature profiles obtained by lidar 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 | 10.15094/00003558 | |||||
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) | |||||
論文名よみ | ||||||
その他のタイトル | Upper stratospheric temperature profiles obtained by lidar at Syowa Station, Antarctica | |||||
著者名(英) |
Nomura, Akio
× Nomura, Akio× Kanzawa, Hiroshi× Kano, Tetsuo |
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著者所属(英) | ||||||
en | ||||||
Faculty of Engineering, Shinshu University | ||||||
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 upper stratospheric temperature profiles in the height range of 20 to 50 km were measured by use of Rayleigh scattering signals obtained at lidar measurements of the sodium layer during the period from March to October, 1985, at Syowa Station (69°00'S, 39°35'E), Antarctica. At first, in order to test the ability of temperature measurement by lidar, the simultaneous co-operative measurements were carried out by lidar, meteorological rocket (MT-135JA), and sonde soundings. The comparison among those results indicated that the temperature profiles obtained by lidar almost agreed with that by rocket sounding in the height range of 20 to 40 km and matched well with that below the height of 20 km by sonde sounding. From the date of 18 nights, it was found that the measured temperature profiles in winter were available because of no disturbance by the aerosol layer which had moved downwards below 25 km as polar stratospheric cloud (PSC). On the other hand, it was found that the profiles in autumn abd spring were partly disturbed by the aerosol layer. | |||||
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 2, p. 8-15, 発行日 1989-08 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |