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Some characteristics of wind and temperature changes in the Syowa Area, Antarctica, in terms of katabatic wind
https://nipr.repo.nii.ac.jp/records/1335
https://nipr.repo.nii.ac.jp/records/1335b3ba343b-42c6-4c22-9eff-d0d780d0b706
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000011969 (1.1 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1982-12-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Some characteristics of wind and temperature changes in the Syowa Area, Antarctica, in terms of katabatic wind | |||||
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 | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Matsubara, Kouji
× Matsubara, Kouji× Ueno, Takeo× Sakamoto, Takahiro× Matsuhara, Kazumasa× Kawaguchi, Sadao |
|||||
著者所属(英) | ||||||
en | ||||||
Japan Meteorological Agency/Japan Meteorological Agency/Japan Meteorological Agency/Japan Meteorological Agency/National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | In order to investigate the characteristics of katabatic wind in the Syowa area, two unmanned weather stations were set up mainly along the flow line of katabatic wind on the coastal zone near Syowa Station (69°00′S, 39°35′E) of East Ongul Island in Lutzow-Holm Bay. One station was installed at the foot of the coastal ice slope and the other on the ice slope 12km inland. From August 1980 to January 1981,wind speed and air temperature were measured at those stations, and vertical soundings by rawinsonde were done at Syowa Station. During the period of increasing of wind speed, a notable difference in wind direction was observed at Syowa Station, and besides, the vertical profiles of temperature and wind were classified into 2 types in terms of the height of inversion layer. When wind direction ranged from ENE to E at Syowa Station, and temperature inversion took place at about 300m high, it was recognized to be a typical katabatic wind. Whereas, on the occasion of wind direction ranged from NNE to NE, inversion layer at 1000m high, and cloudy condition, the wind was identified with that caused by large scale disturbances. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA00733561 | |||||
書誌情報 |
Memoirs of National Institute of Polar Research. Special issue 巻 24, p. 87-93, 発行日 1982-12 |