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RADIO SONDE TEMPERATURE MEASUREMENTS AT DOME FUJI STATION, ANTARCTICA
https://doi.org/10.15094/00004007
https://doi.org/10.15094/0000400739399475-c0c7-4949-bd80-9cb00b55a154
名前 / ファイル | ライセンス | アクション |
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KJ00001014970 (77.6 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1997-11-01 | |||||
タイトル | ||||||
タイトル | RADIO SONDE TEMPERATURE MEASUREMENTS AT DOME FUJI 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 | 10.15094/00004007 | |||||
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 | RADIO SONDE TEMPERATURE MEASUREMENTS AT DOME FUJI STATION, ANTARCTICA | |||||
著者名よみ |
ナカムラ, タツオ
× ナカムラ, タツオ× ヨシミ, ヒデシ× アズマ, ノブヒコ× ヤマノウチ, タカシ |
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著者名(英) |
NAKAMURA, Tatsuo
× NAKAMURA, Tatsuo× YOSHIMI, Hideshi× AZUMA, Nobuhiko× YAMANOUCHI, Takashi |
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著者所属(英) | ||||||
en | ||||||
Kobe Marine Observatory | ||||||
著者所属(英) | ||||||
en | ||||||
Sapporo District Meteorological Observatory | ||||||
著者所属(英) | ||||||
en | ||||||
Nagaoka University of Technology | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Upper air observations using an omega sonde system (RS80-15P : VAISALA) were carried out at Dome Fuji Station from November 7,1995 to January 3,1996. The total number of launched omega sondes was 22. Wind data could not be obtained, because VLF radio waves from omega stations could not be received at Dome Fuji Station. Seven omega sondes reached the tropopause, but the others failed due to problems with the sondes or the receiving apparatus. The average maximum height the sonde reached was about 8km above sea level. A remarkable inversion layer was found with 21 observations. The maximum temperature difference between the top and bottom of the layer was 17.8℃. The mean thickness (ΔH) of the inversion layer was 256m and the mean temperature difference (ΔT) between the top and bottom of the layer was 6.8℃. The observations show that ΔT is largest between 03 LT and 09 LT, and ΔH is thinnest between 21 LT and 03 LT. | |||||
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 11, p. 259, 発行日 1997-11 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |