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INTERANNUAL VARIATIONS OF ZONAL MEAN TEMPERATURE IN THE SOUTHERN HEMISPHERE STRATOSPHERE : WITH REFERENCE TO THE ANTARCTIC OZONE DEPLETION
https://doi.org/10.15094/00003520
https://doi.org/10.15094/000035206ca82bcc-d770-494a-b4ce-8b7af16165a6
名前 / ファイル | ライセンス | アクション |
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KJ00000767728 (1.1 MB)
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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 | INTERANNUAL VARIATIONS OF ZONAL MEAN TEMPERATURE IN THE SOUTHERN HEMISPHERE STRATOSPHERE : WITH REFERENCE TO THE ANTARCTIC OZONE DEPLETION | |||||
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 | 10.15094/00003520 | |||||
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 | INTERANNUAL VARIATIONS OF ZONAL MEAN TEMPERATURE IN THE SOUTHERN HEMISPHERE STRATOSPHERE : WITH REFERENCE TO THE ANTARCTIC OZONE DEPLETION | |||||
著者名よみ |
カワヒラ, コウジ
× カワヒラ, コウジ× ヒロオカ, トシヒコ |
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著者名(英) |
KAWAHIRA, Kohji
× KAWAHIRA, Kohji× HIROOKA, Toshihiko |
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著者所属(英) | ||||||
en | ||||||
Geophysical Institute, Faculty of Science, Kyoto University:(Present address)Toyama National College of Technology | ||||||
著者所属(英) | ||||||
en | ||||||
Geophysical Institute, Faculty of Science, Kyoto University:(Present address)Numerical Prediction Division, Japan Meteorological Agency | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Interannual variations of the zonal mean temperature in the Antarctic lower stratosphere are analyzed for the past six years from 1980 to 1985 by using NMC data. It is found that the Antarctic polar stratosphere tends to cool not only in spring but also in all seasons, remarkably in the polar region. The analysis of the meridional gradient of the zonal mean temperature shows such an interesting feature that the period of temperature decrease toward the pole in winter has become longer and longer in recent years in accord with the Antarctic ozone depletion. From these evidences, the interrelation between the temperature decline and the ozone depletion is considered as follows : Slight cooling induced by the effect of increasing CO_2 can form the polar stratospheric clouds, and more clouds are formed by its radiative cooling effect. Hence, enhanced cooling in the polar region can induce the ozone depletion due to less poleward transport of ozone by planetary waves, which become less active in the polar region due to trapping by long-persistent strong westerlies. | |||||
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. 31-38, 発行日 1987-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |