Item type |
紀要論文(ELS) / Departmental Bulletin Paper(1) |
公開日 |
1992-02-01 |
タイトル |
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タイトル |
BARE ICE FIELDS DEVELOPED IN THE INLAND PART OF ANTARCTICA |
言語 |
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言語 |
eng |
資源タイプ |
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資源タイプ識別子 |
http://purl.org/coar/resource_type/c_6501 |
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資源タイプ |
departmental bulletin paper |
ID登録 |
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ID登録 |
10.15094/00003706 |
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ID登録タイプ |
JaLC |
ページ属性 |
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内容記述タイプ |
Other |
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内容記述 |
P(論文) |
論文名よみ |
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その他のタイトル |
BARE ICE FIELDS DEVELOPED IN THE INLAND PART OF ANTARCTICA |
著者名よみ |
タカハシ, シュウヘイ
エンドウ, タツオ
アズマ, ノブヒコ
メシダ, シゲミ
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著者名(英) |
TAKAHASHI, Shuhei
ENDOH, Tatsuo
AZUMA, Nobuhiko
MESHIDA, Shigemi
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著者所属(英) |
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en |
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Kitami Institute of Technology |
著者所属(英) |
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en |
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Institute of Low Temperature Science, Hokkaido University |
著者所属(英) |
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en |
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Faculty of Technology, Hokkaido University:(Present address)Nagaoka Technology and Science Institute |
著者所属(英) |
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en |
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Japan Meteorological Agency |
抄録(英) |
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内容記述タイプ |
Other |
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内容記述 |
Observations of a bare ice field was carried out at Seal Rock in the S∅r Rondane area, East Antarctica. A large sublimation rate, 200 to 280mm/a, was observed on the bare ice field. Air temperature on the bare ice was about 1℃ higher than that on snow surface. The large sublimation rate was explained from the low albedo of bare ice; its value was roughly estimated from heat budget considerations. The bare ice fields were classified into 4 types according to origin. |
雑誌書誌ID |
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収録物識別子タイプ |
NCID |
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収録物識別子 |
AA10756213 |
書誌情報 |
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
巻 5,
p. 128-139,
発行日 1992-02
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出版者 |
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出版者 |
National Institute of Polar Research |