Observation of snow drift flux at Mizuho Station, East Antarctica, 1982
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概要
- 論文の詳細を見る
Continuous observation of snow drift flux was carried out at Mizuho Station (70°42′S, 44°20′E, 2230m above sea level), East Antarctica, in 1982. Snow drift flux at 1m height was well correlated with wind velocity. The correlation coefficient on a logarithmic plot was between 0.8 and 0.9. The drift flux was proportional to about the 8 power of wind velocity through the year. The power decreased above -20℃. The drift flux increased when precipitation was observed. From the variation of drift flux, precipitation intensity can be estimated.
- 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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Nishio Fumihiko
National Institute Of Polar Research
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Ishikawa Masao
The Institute Of Low Temperature Science Hokkaido University
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Ohmae Hirokazu
The Institute Of Low Temperature Science Hokkaido University:(present Address)space Development Prom
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Ohmae Hirokazu
The Institute Of Low Temperature Science Hokkaido University
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Nishio F
Chiba Univ. Chiba
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Katsushima Takayoshi
Faculty of Science, Hokkaido University
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Katsushima Takayoshi
Department Of Geology And Mineralogy Faculty Of Science Hokkaido University
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