BARE ICE FIELDS DEVELOPED IN THE INLAND PART OF ANTARCTICA
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概要
- 論文の詳細を見る
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.
- 国立極地研究所の論文
著者
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Takahashi Shuhei
Kitami Institute of Technology
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Azuma Nobuhiko
Faculty Of Technology Hokkaido University:(present Address)nagaoka Technology And Science Institute
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ENDOH Tatsuo
Institute of Low Temperature Science, Hokkaido University
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Endoh Tatsuo
Institute Of Low Temperature Science Hokkaido Univ.
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Meshida Shigemi
Japan Meteorological Agency
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