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Abstract
According to the characteristics of sodar echo,a classified method for temperature stratification is given.By using sodar data observed in Yanshan Mountain area in Beijing,the statistical characteristics for the height of inversion layer,thermal plume,and the depth of mixed layer are compared.Finally,the appearance frequency for stable,unstable and neutral stratification is analyzed.
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Citation
LüNaiping, Zhou Mingyu, Su Lirong, Chen Yanjuan. 1989: A STATISTICAL ANALYSIS OF SODAR DATA DETECTED IN YANSHAN MOUNTAIN AREA,BEIJING. Journal of Meteorological Research, 3(5): 645-652.
LüNaiping, Zhou Mingyu, Su Lirong, Chen Yanjuan. 1989: A STATISTICAL ANALYSIS OF SODAR DATA DETECTED IN YANSHAN MOUNTAIN AREA,BEIJING. Journal of Meteorological Research, 3(5): 645-652.
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LüNaiping, Zhou Mingyu, Su Lirong, Chen Yanjuan. 1989: A STATISTICAL ANALYSIS OF SODAR DATA DETECTED IN YANSHAN MOUNTAIN AREA,BEIJING. Journal of Meteorological Research, 3(5): 645-652.
LüNaiping, Zhou Mingyu, Su Lirong, Chen Yanjuan. 1989: A STATISTICAL ANALYSIS OF SODAR DATA DETECTED IN YANSHAN MOUNTAIN AREA,BEIJING. Journal of Meteorological Research, 3(5): 645-652.
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