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RESULTS OF OZONE OBSERVATION FROM THE EQUATORIAL REGION TO ANTARCTICA IN 1987
https://doi.org/10.15094/00003637
https://doi.org/10.15094/00003637b2139c05-ad6c-444c-8ac2-7beb20f268fa
名前 / ファイル | ライセンス | アクション |
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KJ00000767840 (1.7 MB)
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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 | RESULTS OF OZONE OBSERVATION FROM THE EQUATORIAL REGION TO ANTARCTICA IN 1987 | |||||
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 | 10.15094/00003637 | |||||
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 | RESULTS OF OZONE OBSERVATION FROM THE EQUATORIAL REGION TO ANTARCTICA IN 1987 | |||||
著者名よみ |
マツバラ, コウジ
× マツバラ, コウジ× ドイ, モトヒサ× ウエクボ, テツロウ× オカダ, ケンジ× アオキ, シュンジ× カワグチ, サダオ |
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著者名(英) |
MATSUBARA, Kouji
× MATSUBARA, Kouji× DOI, Motohisa× UEKUBO, Tetsuro× OKADA, Kenji× AOKI, Shuhji× KAWAGUCHI, Sadao |
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著者所属(英) | ||||||
en | ||||||
Japan Meteorological Agency | ||||||
著者所属(英) | ||||||
en | ||||||
Japan Meteorological Agency | ||||||
著者所属(英) | ||||||
en | ||||||
Japan Meteorological Agency | ||||||
著者所属(英) | ||||||
en | ||||||
Japan Meteorological Agency | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The first total ozone observation and vertical ozone sounding on board the research vessel 'SHIRASE' from the equatorial region to Antarctica was carried out in 1987 by meteorological members of the 29th JARE (Japanese Antarctic Research Expedition) team. Total ozone and vertical ozone profile were measured by Brewer ozone spectrophotometer and ozonesondes, respectively. The detailed latitudinal distribution of total ozone amount and height-latitude distributions of ozone concentration, temperature and wind at 5-degree latitude intervals from the equatorial region to the Antarctic region were observed. From the ozonesonde observations, the injection of ozone from the stratosphere to the troposphere through the tropopause gap was deduced. The decreased ozone concentration in the lower stratosphere, similar to as same as the Antarctic ozone hole, was observed south of 60°S. It is possible that this phenomenon was caused by transport of ozone-poor air (a 'dilution effect') following the spring time ozone hole. | |||||
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. 1-11, 発行日 1991-05 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |