Ultraviolet Radiation in Overcast Sky at the Surface

Based on the analysis of one year of observation data of solar radiation at the ground in Beijing in 1990, a simple empirical formula for calculating UV radiation in overcast sky is established. The formula is Quv/Quv0 = A1S + A0, where Quv and Quvo are monthly mean daily sums of UV exposure in overcast sky and clear sky, respectively. S is the daily sunshine hours. The calculated results agree well with the observed. The maximum and minimum relative biases are 9.9% and 0.1%, respectively, and the yearly relative bias is 2.9%. The ratio of ultraviolet radiation of overcast sky to clear sky in 1990 is between 44.6% and 61.8%, and the yearly average is 53.9%. Thus, almost half of the UV energy is lost in the atmosphere in overcast sky in 1990.

作 者： 自建輝 王庚辰 胡非   作者單位： 自建輝(Laboratory for Middle Atmosphere Layer and Global Environment Observation,Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029;State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry,Institute of Atmos)

王庚辰(Laboratory for Middle Atmosphere Layer and Global Environment Observation,Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029)

胡非(State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry,Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029) 

刊 名： 大氣科學(xué)進展(英文版)  ISTIC SCI 英文刊名： ADVANCES IN ATMOSPHERIC SCIENCES  年，卷(期)： 2003 20(6)  分類號：   關(guān)鍵詞： ultraviolet radiation   overcast sky   sunshine hours   cloudiness  

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