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Dependence of oxygen isotopic composition of surface snow on distance from coast in Mizuho Plateau
https://nipr.repo.nii.ac.jp/records/1342
https://nipr.repo.nii.ac.jp/records/13427c63b3fd-14c6-44bf-bc47-015f84e0b86a
名前 / ファイル | ライセンス | アクション |
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KJ00000011976.pdf (680.8 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1982-12-01 | |||||
タイトル | ||||||
タイトル | Dependence of oxygen isotopic composition of surface snow on distance from coast in Mizuho Plateau | |||||
言語 | en | |||||
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 | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Higuchi, Keiji
× Higuchi, Keiji |
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著者所属(英) | ||||||
言語 | en | |||||
値 | Water Research Institute, Nagoya University | |||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The dependency of the δ^<18>O values of drifting snow on distance from the coast was studied on the basis of the data obtained by the traverse of the 15th Japanese Antarctic Research Expedition in 1974. The rate of horizontal variation of the δ^<18>O value was 7.5 and 7.8‰/100km in the coastal region, and 4.2 and 5.0‰/100km in the inland region. On the basis of a simple model of the precipitation process, it can be said from the rate of horizontal variation of the δ^<18>O values that precipitation in the coastal region is from convective clouds with large vertical velocity and precipitation in the inland region is from clouds related to synoptic scale disturbances with small vertical velocity. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA00733561 | |||||
書誌情報 |
Memoirs of National Institute of Polar Research. Special issue 巻 24, p. 122-126, 発行日 1982-12 |