臭氧变化及其气候效应研究进展

Wang Tijian, Sun Zhaobo
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引用次数: 5

摘要

本文综述了近年来臭氧变化的特征、机理及其气候效应的研究进展。对流层(北半球)臭氧量呈增加趋势,平流层臭氧量呈减少趋势,臭氧总量呈减少趋势,显示出全球臭氧变化的趋势。主要原因是由于人类活动导致NOx、NMHC、CO、ch4等o3前体物质增加,破坏平流层o3的物质(NOx、h2o、n2o、cfc)增加。对流层臭氧的增强会使地表和低层大气变暖,而平流层臭氧的耗竭会使地表和低层大气变暖或变冷。将全球或区域气候模式与大气化学模式相结合是研究臭氧变化及其气候效应的一种非常有效的方法。
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DEVELOPMENT OF STUDY ON OZONE VARIATION AND ITS CLIMATIC EFFECT
In this paper,the developments of study on characteristics and mechanism of ozone variation and its climate effect are reviewed.The amount of tropospheric O 3(in North Hemisphere)is increasing,that of stratospheric O 3 is decreasing and the total ozone amount also is decreasing which show the trend of global ozone variation.The main reason is that the O 3 precusors,such as NOx,NMHC,CO,CH 4,are increasing due to human activities and the species(NOx,H 2O,N 2O,CFCs)which can destroy stratospheric O 3 are increasing.The enhancement of tropospheric O 3 will warm the ground surface and the lower atmosphere and the depletion of stratospheric O 3 may warm or cool the ground surface and lower atmosphere.It is a very effective way to use the global or regional climate model coupled with a atmospheric chemistry model for study on ozone variation and its climate effect.
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