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HOW GRAVITY WAVES AFFECT FORMATION OF LOW TEMPERATURE REGION IN ANTARCTIC LOWER STRATOSPHERE
https://doi.org/10.15094/00003522
https://doi.org/10.15094/00003522c5b44c48-adad-4d4e-ba53-8d3b17133e63
名前 / ファイル | ライセンス | アクション |
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KJ00000767730 (576.6 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 | HOW GRAVITY WAVES AFFECT FORMATION OF LOW TEMPERATURE REGION IN ANTARCTIC LOWER STRATOSPHERE | |||||
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 | 10.15094/00003522 | |||||
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 | HOW GRAVITY WAVES AFFECT FORMATION OF LOW TEMPERATURE REGION IN ANTARCTIC LOWER STRATOSPHERE | |||||
著者名よみ |
タナカ, ヒロシ
× タナカ, ヒロシ |
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著者名(英) |
TANAKA, Hiroshi
× TANAKA, Hiroshi |
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著者所属(英) | ||||||
en | ||||||
Water Research Institute, Nagoya University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | A mechanism is proposed for the formation of an "ozone hole" over Antarctica. Gravity waves emitted from the circum-continental mountain (or cliff) belt may be partly saturated in the lower stratosphere and suppress planetary wave activity there. This process results in shielding a poleward heat transport associated with planetary waves. A long-term trend of gravity wave activity and prevailing wind system for the past several years should be detected in the polar region. | |||||
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. 54-58, 発行日 1987-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |