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Such annual variation is compared with that of surface snow drift collected at Mizuho Station (70.7°S, 44.3°E) through the year, since deposited snow is composed of accumulated snow drift. The δ^\u003c18\u003eO contents in the snow drift had high values in summer (-30\u0026acd; -40‰); in winter, values were generally low (above -50‰) but sometimes there were high values similar to those in summer. The annual range of those was about 20‰. It can be seen in relations between air temperature at sampling time and δ^\u003c18\u003eO contents in the snow drift during snowfall, blowing snow and no snowfall, that the temperature during blowing snow tends to be higher and the temperature during no snowfall tends to be lower, compared with that during snowfall at similar δ^\u003c18\u003eO content of the snow drift. Consequently, vertical profiles of oxygen isotopic contents of accumulated snow drift are supposed to show a wide annual range and complicated annual variation. However, those of deposited snow actually seen in the surface layer usually show a narrow range and simplified pattern. 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OXYGEN ISOTOPE PROFILES OF DEPOSITED SNOW IN DIFFERENT DEPOSITIONAL ENVIRONMENTS OF THE ANTARCTIC ICE SHEET-II
https://doi.org/10.15094/00003757
https://doi.org/10.15094/00003757bb58ce28-7ae1-450f-b623-0e55c258281b
名前 / ファイル | ライセンス | アクション |
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KJ00000767911 (61.2 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1992-12-01 | |||||
タイトル | ||||||
タイトル | OXYGEN ISOTOPE PROFILES OF DEPOSITED SNOW IN DIFFERENT DEPOSITIONAL ENVIRONMENTS OF THE ANTARCTIC ICE SHEET-II | |||||
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 | 10.15094/00003757 | |||||
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 | OXYGEN ISOTOPE PROFILES OF DEPOSITED SNOW IN DIFFERENT DEPOSITIONAL ENVIRONMENTS OF THE ANTARCTIC ICE SHEET-II | |||||
著者名よみ |
アゲタ, ユタカ
× アゲタ, ユタカ× カミヤマ, コキチ |
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著者名(英) |
AGETA, Yutaka
× AGETA, Yutaka× KAMIYAMA, Kokichi |
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著者所属(英) | ||||||
en | ||||||
Water Research Institute, Nagoya University | ||||||
著者所属(英) | ||||||
en | ||||||
Beppu Geophysical Research Laboratory Faculty of Science, Kyoto University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | In the region between Dome F (77.4°S, 39.6°E) and the Princess Astrid Coast, annual variation of oxygen isotopic contents in vertical profiles of deposited snow cannot be seen in the inland plateau due to low accumulation rates, but it can be seen in the coastal area below the north slope of the S∅r Rondane Mountains. Such annual variation is compared with that of surface snow drift collected at Mizuho Station (70.7°S, 44.3°E) through the year, since deposited snow is composed of accumulated snow drift. The δ^<18>O contents in the snow drift had high values in summer (-30∿ -40‰); in winter, values were generally low (above -50‰) but sometimes there were high values similar to those in summer. The annual range of those was about 20‰. It can be seen in relations between air temperature at sampling time and δ^<18>O contents in the snow drift during snowfall, blowing snow and no snowfall, that the temperature during blowing snow tends to be higher and the temperature during no snowfall tends to be lower, compared with that during snowfall at similar δ^<18>O content of the snow drift. Consequently, vertical profiles of oxygen isotopic contents of accumulated snow drift are supposed to show a wide annual range and complicated annual variation. However, those of deposited snow actually seen in the surface layer usually show a narrow range and simplified pattern. This difference suggests the importance of change of isotopic content after snow deposition for understanding oxygen isotope profiles of deposited snow. | |||||
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 6, p. 154, 発行日 1992-12 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |