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MID-WINTER WARMINGS IN THE SOUTHERN HEMISPHERE STRATOSPHERE IN 1988
https://doi.org/10.15094/00003650
https://doi.org/10.15094/000036504a75765f-1de3-4f44-aed8-aaf2f9c6336b
名前 / ファイル | ライセンス | アクション |
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KJ00000767853 (106.9 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1991-05-01 | |||||
タイトル | ||||||
タイトル | MID-WINTER WARMINGS IN THE SOUTHERN HEMISPHERE STRATOSPHERE IN 1988 | |||||
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 | 10.15094/00003650 | |||||
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 | MID-WINTER WARMINGS IN THE SOUTHERN HEMISPHERE STRATOSPHERE IN 1988 | |||||
著者名よみ |
シオタニ, マサト
× シオタニ, マサト× ヒロタ, イサム× クロイ, ケイコ× ヒラキ, トオル |
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著者名(英) |
SHIOTANI, Masato
× SHIOTANI, Masato× HIROTA, Isamu× KUROI, Keiko× HIRAKI, Tooru |
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著者所属(英) | ||||||
en | ||||||
Department of Geophysics, Faculty of Science, Kyoto University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Geophysics, Faculty of Science, Kyoto University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Geophysics, Faculty of Science, Kyoto University | ||||||
著者所属(英) | ||||||
en | ||||||
Japan Meteorological Agency | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | An analysis was done of intense midwinter warmings which took place in the southern hemisphere stratosphere during August-September 1988. By using the southern hemispheric data set up to the 1 mb level provided by Japan Meteorological Agency, it is found that the 30 mb temperature increase over eastern Antarctica, about 60 K for 10 days from August 22 to September 1,is associated with the amplification of a quasi-stationary planetary wave of zonal wavenumber 1. The enhancement of wave 1 appears quasi-periodically with a times scale of about 2 weeks during the mid-winter of 1988. Clear evidence is presented to show that the quasi-periodic amplification of wave 1 is due to the wave-wave interaction between the quasi-stationary forced wave of wavenumber 1 and the eastward traveling wave of wavenumber 2. It is emphasized, therefore, that the mechanism of warming in this case is quite different from the transient vertical propagation of a planetary wave forced from below as observed in the northern hemisphere winter. | |||||
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 4, p. 119, 発行日 1991-05 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |