摘要
平流层臭氧的变化对平流层的温度结构、整个大气环流以及到达地面的紫外辐射均有影响。本文采用一个计算臭氧吸收太阳辐射的参数化方法和有关资料，研究了臭氧变化对大气最大加热率和到达地面的紫外辐射通量密度的影响情况。文中给出的参数化方法可直接应用于大气环流模式计算臭氧吸收太阳辐射的加热率。
The changes of ozt)n6 in stratosphere affect the temperature strucTure of straosphere, theatmospheric circulation and the ultraviolet ratliation received at the earth' s surface. A param-eterization method of computing the solar radiation absorbed by ozone is used to study the effc ts of ozone fhanges on the maximum heating rate and the ultraviolef radiation received atthe earth' S surface. The method can ba applied to the atmospheric circulation model to calcu-late the heating rate.
出处
《气象科学》
CSCD
北大核心
1997年第1期71-82,共12页
Journal of the Meteorological Sciences
