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A stratification model of surface snow at Dome Fuji Station, Antarctica
https://kitami-it.repo.nii.ac.jp/records/7188
c446030c-f7c5-4336-9ed2-f53ad613eed1
名前 / ファイル | ライセンス | アクション | |
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2007-06-13 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | A stratification model of surface snow at Dome Fuji Station, Antarctica | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | journal article | |||||
アクセス権 | ||||||
アクセス権 | open access | |||||
アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||
著者 |
Zhou, Yiying
× Zhou, Yiying× Azuma, Nobuhiko× Kameda, Takao |
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著者別名 | ||||||
姓名 | ||||||
姓名 | 亀田, 貴雄 | |||||
言語 | ja | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | A stratification model of surface snow on the ice sheet, which includes snow density evolution, is proposed. Using the temperature profile in the surface snow layer obtained at Dome Fuji Station, Antarctica, snow density evolution under various accumulation conditions was simulated.It is demonstrated that water vapor diffusion is very important for the snow density evolution, and temperature and accumulation at the snow surface are the most important factors that determine the future snow density profile below the surface. | |||||
書誌情報 |
Polar Meteorology and Glaciology 巻 16, p. 61-73, 発行日 2002-11 |
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権利 | ||||||
権利情報 | NATIONAL INSTITUTE OF POLAR RESEARCH, Y. Zhou, N. Azuma, T. Kameda, Polar Meteorology and Glaciology, 16, 2002, 61-73. | |||||
フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | application/pdf | |||||
出版者 | ||||||
出版者 | 国立極地研究所 | |||||
著者版フラグ | ||||||
値 | publisher | |||||
出版タイプ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |