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TEMPORAL AND SPATIAL FLUCTUATIONS OF WARMING IN ANTARCTICA AND THE ATMOSPHERIC CIRCULATION
https://doi.org/10.15094/00004010
https://doi.org/10.15094/00004010f4675a96-fcd2-44fc-836d-a5b743b471c2
名前 / ファイル | ライセンス | アクション |
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KJ00001014973 (86.4 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 | TEMPORAL AND SPATIAL FLUCTUATIONS OF WARMING IN ANTARCTICA AND THE ATMOSPHERIC CIRCULATION | |||||
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 | 10.15094/00004010 | |||||
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 | TEMPORAL AND SPATIAL FLUCTUATIONS OF WARMING IN ANTARCTICA AND THE ATMOSPHERIC CIRCULATION | |||||
著者名よみ |
エノモト, ヒロユキ
× エノモト, ヒロユキ |
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著者名(英) |
ENOMOTO, Hiroyuki
× ENOMOTO, Hiroyuki |
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著者所属(英) | ||||||
en | ||||||
Kitami Institute of Technology | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | An abrupt and extreme warming was observed in the mid-winter season, in June 1994. The air temperature increased from -72℃ to -36℃ in two days. This warming caused reduced cooling of air temperature in the winter and hence resulted in increase of the temperature throughout a month. The area of warming and its temperature change were analyzed by using the passive microwave radiometer (DMSP SSM/I) data. This area appeared first in the coastal region around the Lambert Glacier, East Antarctica and expanded to the inland areas over Dome Fuji, then diminished over the Dome C area. The weather chart showed a high pressure area over East Antarctica, and advection of air from the coastal region to the inland areas of Antarctica. A blocking of high pressure was detected in the higher troposphere and persisted for several weeks. The seasonal variations of the polar vortex in the stratosphere (30hPa) showed a westward shift of the center area in the corresponding period. This event is important to understand the Antarctic climate and also exchange processes of polar air masses. | |||||
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. 261, 発行日 1997-11 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |