与高层大气臭氧层不同的是，地面的臭氧是光化学烟雾的一个主要组成部分。
Ozone at ground level - not to be confused with the ozone layer in the upper atmosphere - is one of the major constituents of photochemical smog.
由于光化过程，在平流层与中层内产生了臭氧。
Ozone is formed in the stratosphere and mesosphere by photochemical processes.
借助OH夜气辉辐射的光化学模式，由OH夜气辉辐射反演中间层-低热层区域的原子氧数密度时，输入参数的不确定性将导致反演得到的原子氧数密度具有不确定性。
When the atomic oxygen density in the mesosphere and lower thermosphere region is derived by means of photochemical model calculations from OH nightglow emissions, a retrieval uncertainty, I.
局地光化学生成是白天边界层o3的主要来源；降水天气过程可造成O3及其前体物浓度的显著变化。
It was also found that the photochemistry reaction was an important source in boundary layer in daytime and precipitation process could arouse marked change of O3 concentration.
甲烷的光化学氧化可能是大气对流层有机过氧化物的重要来源。
Photooxidation of CH4 probably was an important source of organic peroxides in the troposphere.
甲烷的光化学氧化可能是大气对流层有机过氧化物的重要来源。
Photooxidation of CH4 probably was an important source of organic peroxides in the troposphere.
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