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《PLATEAU METEOROLOGY》 1998-02
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THE EFFECTS OF AEROSOL AND WATER-VAPOUR’Se-TYPE ABSORPTION ON LOWER ATMOSPHERICLONG-WAVE COOLING RATES

SU Wen-ying CHEN Chang-he(Department of Atmospheric Science of Lanzhou University,Lanzhou, Gansu 730000)  
In this paper, we use the band model to calculate the atmospheric long-wave cooling rates. The results show in the lower atmosphere, the cooling rate of the water vapour e-type absorption of window region is less than that of non-window region and is about 1/3 of the total water vapour cooling rate. The long-wave cooling rate of aerosol is less than that of water vapour and its contribution to total atmospheric cooling rate is about 30%. The distribution of total cooling rate in the lower atmosphere is mainly determined the distribution of water vapor cooling rate.
【Fund】: 国家自然科学基金
【CateGory Index】: P422.3
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1 Su Wenying1 Chen Changhe2 ( 1 Department of Geophysics of Beijing University,LSSR,Beijing 100871)( 2 Department of Atmospheric Science of Lanzhou University,Lanzhou,Gansu 730000));THE EFFECTS OF AEROSOL OPTICAL ABSORPTION CHARACTERISTICS ON LOWER ATMOSPHERIC HEATING RATES[J];Plateau Meteorology;1997-04
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