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CHEMISTRY OF SNOW, AEROSOLS AND ATMOSPHERIC ACID GAS AT DOME FUJI STATION, ANTARCTICA
https://doi.org/10.15094/00003986
https://doi.org/10.15094/00003986506da200-212c-4286-95a1-8ed33e2d863d
名前 / ファイル | ライセンス | アクション |
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KJ00001014949 (76.3 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1997-11-01 | |||||
タイトル | ||||||
タイトル | CHEMISTRY OF SNOW, AEROSOLS AND ATMOSPHERIC ACID GAS AT DOME FUJI STATION, 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 | 10.15094/00003986 | |||||
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 | CHEMISTRY OF SNOW, AEROSOLS AND ATMOSPHERIC ACID GAS AT DOME FUJI STATION, ANTARCTICA | |||||
著者名よみ |
カナモリ, サトル
× カナモリ, サトル× カナモリ, ノブコ× ワタナベ, オキツグ× カメダ, タカオ |
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著者名(英) |
KANAMORI, Satoru
× KANAMORI, Satoru× KANAMORI, Nobuko× WATANABE, Okitsugu× KAMEDA, Takao |
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著者所属(英) | ||||||
en | ||||||
Nagoya University | ||||||
著者所属(英) | ||||||
en | ||||||
Nagoya University | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
著者所属(英) | ||||||
en | ||||||
Kitami Institute of Technology | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | A year-round sampling of surface snow, aerosols (using 0.2μm Nuclepore filter) and acid gases (using alkali impregnated filter) was carried out at Dome Fuji Station in the period from February to December of 1995 by the 36th JARE. Samples were transported under refrigeration. The concentration levels of exSO_4^<2->, MSA, NO_3^-, Cl^-, NH_4^+, Na^+ and K^+ in snow at Dome Fuji Station are nearly comparable to those observed on the Mizuho Plateau, especially with those at elevation higher than ca. 3500m. And further, the patterns of seasonal variation of exSO_4^<2->, MSA and NO_3^- in aerosols taken at Dome Fuji Station, high in summer and low in winter, are similar to those at Syowa Station. These observations lead to an impression of the same source and transport mechanism of non-sea salt components in snow and aerosols on the Dome Fuji and in Mizuho Plateau. However, strikingly, the concentrations of non-sea salt components in the aerosols taken at DomeFuji Station were as low as several hundredths of those observed at Syowa Station or on the Mizuho Plateau. This may suggest a different manner of incorporating chemical components into snow and, therefore, into glacier ice. More observations are needed before reaching a firm conclusion. | |||||
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 11, p. 242, 発行日 1997-11 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |