摘要
本文利用北京地区1980—1986年的臭氧和高空资料,讨论了臭氧总量的突变过程及其与高空气温的关系,发现:北京地区臭氧总量的突变过程全部发生在冬、春季节;随着臭氧总量的突增,对流层的气温呈下降趋势,平流层的气温呈、上升趋.势;气温变化与臭氧总量变化之间负相关和正相关最好的层欢分别为500hPa和70hPa,它们的相关系数,分别为-0.85和0.63。
The ozone and aerological sounding data during 1980-1986 in Beijing area are used to discuss the abrupt variations of the total ozone and its relationship with the changes of the upper air temperature.The results are: 1. All processes of the abrupt variations of the total ozone in Beijing area take place in springs and winters. 2. With the sudden increase of the total ozone, there is temperature decrease in the troposphere but an increase in the stratosphere. 3. The levels where the variations of the air temperature and the total ozone show their best negative or positive correlation are 500hPa and 70hPa, and their correlation coefficients are -0.85 and 0.63 respectively.
出处
《气象》
CSCD
北大核心
1990年第4期15-18,共4页
Meteorological Monthly
