Calculation of heating rate in the Antarctic stratosphere in 1985 using SAGE II data
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概要
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The radiative heating effects due to molecules and aerosols over Antarctica during September-October 1985 have been examined, by using a detailed radiative transfer scheme and SAGE II data. In the calculation of radiative transfer, we have considered the absorption of solar radiation, the atmospheric thermal emission and absorption, Rayleigh and Mie scatterings, and the surface scattering effects. The results show that the heating rate in the Antarctic stratosphere during that period is too small to cause effective upward motions, even if aerosol heating is included.
- 国立極地研究所の論文
著者
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FUJIWARA Motowo
Department of Earth System Science, Faculty of Science, Fukuoka University
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Akiyoshi Hideharu
Department Of Applied Physics Fukuoka University
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Akiyoshi Hideharu
Department Of Physics Faculty Of Science Kyushu University
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Fujiwara Motowo
Department Of Applied Physics Faculty Of Science Fukuoka University
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Uryu Michiya
Department of Physics, Faculty of Science, Kyushu University
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Uryu Michiya
Department Of Physics Faculty Of Science Kyushu University
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