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ATMOSPHERIC NITROGEN DIOXIDE IN ANTARCTICA
https://doi.org/10.15094/00003534
https://doi.org/10.15094/0000353402a92e54-f2f3-47f2-802d-525cb58cb685
名前 / ファイル | ライセンス | アクション |
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KJ00000767742 (109.1 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 | ATMOSPHERIC NITROGEN DIOXIDE IN ANTARCTICA | |||||
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 | 10.15094/00003534 | |||||
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 | ATMOSPHERIC NITROGEN DIOXIDE IN ANTARCTICA | |||||
著者名よみ |
シバサキ, カズオ
× シバサキ, カズオ× オガワ, トシヒロ× イワガミ, ナオモト |
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著者名(英) |
SHIBASAKI, Kazuo
× SHIBASAKI, Kazuo× OGAWA, Toshihiro× IWAGAMI, Naomoto |
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著者所属(英) | ||||||
en | ||||||
Kokugakuin University | ||||||
著者所属(英) | ||||||
en | ||||||
Geophysics Research Laboratory, Faculty of Science, University of Tokyo | ||||||
著者所属(英) | ||||||
en | ||||||
Geophysics Research Laboratory, Faculty of Science, University of Tokyo | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Seasonal behavior of stratospheric NO_2 content was determined for the period of March 1983 to January 1984 from ground-based spectroscopic measurements at Syowa Station. The winter minimum of about 1×(10)^<15>(cm)^<-2> and the summer maximum of about 7×(10)^<15>(cm)^<-2> were observed. This seasonal behavior compares well with those observed at northern high latitudes. A rapid increase in column density started at the end of September before the minimum of total ozone in mid-October. This increase in column density seems to correlate with an increase in sunlit time in the stratosphere. Our results imply that both dynamical and photochemical processes may be involved in the Antarctic ozone depletion. The first balloon observation of stratospheric NO_2 profile in Antarctica was made on November 24,1982 and two observations on November 12 and 20,1983 at Syowa Station. All observations were concentrated in November, early summer in Antarctica. Two vertical profiles, sunset and sunrise ones, could be deduced in series from one balloon flight. They should be virtually the same rather than corresponding to different profiles for the evening and morning, because, in this season of year, the sunlit condition lasted all day long at the balloon altitude. No quantitative change can be seen in profiles between 1982 and 1983. Above 25km altitude, three profiles are basically identical to those observed at middle and high latitudes in the northern hemisphere. | |||||
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. 147, 発行日 1987-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |