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INFLUENCES OF ARCTIC OZONE HOLE ON THE STRATOSPHERIC GENERAL CIRCULATION
https://doi.org/10.15094/00002884
https://doi.org/10.15094/000028845488194f-199e-452c-8746-0d07c89cc5a8
名前 / ファイル | ライセンス | アクション |
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KJ00002409899 (1.2 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1999-12-01 | |||||
タイトル | ||||||
タイトル | INFLUENCES OF ARCTIC OZONE HOLE ON THE STRATOSPHERIC GENERAL 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 | 10.15094/00002884 | |||||
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 | ||||||
Scientific Paper | ||||||
論文名よみ | ||||||
その他のタイトル | INFLUENCES OF ARCTIC OZONE HOLE ON THE STRATOSPHERIC GENERAL CIRCULATION | |||||
著者名よみ |
ヒロオカ, トシヒコ
× ヒロオカ, トシヒコ× ニシヨシ, トシヒコ× ワタナベ, シンゴ× ミヤハラ, サブロウ |
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著者名(英) |
HIROOKA, Toshihiko
× HIROOKA, Toshihiko× NISHIYOSHI, Toshihiko× WATANABE, Shingo× MIYAHARA, Saburo |
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著者所属(英) | ||||||
en | ||||||
Department of Earth and Planetary Sciences, Kyushu University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Earth and Planetary Sciences, Kyushu University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Earth and Planetary Sciences, Kyushu University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Earth and Planetary Sciences, Kyushu University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Numerical experiments are performed for four years to estimate radiative and dynamical influences of the "Arctic ozone hole" on the stratospheric general circulation by using a general circulation model developed at Kyushu University. The model includes simplified ozone photochemistry interactively coupled with radiation and dynamics. The resultant temperature structure consists of cooling of about 6K in the polar lower stratosphere and warming of about 8K in the polar upper stratosphere, which intensifies the polar night jet by about 9ms^<-1>. The cooling is caused by reduction of downward motion as well as decrease of solar UV heating due to ozone depletion, while the warming is caused by dynamical heating due to enhancement of downward motion. The results imply that the feedback mechanism may strengthen the ozone hole itself. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1129795X | |||||
書誌情報 |
Polar meteorology and glaciology 巻 13, p. 1-10, 発行日 1999-12 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |