NUMREICAL SIMULATION OF THE SEASONAL VARIATION OF TROPOSPHERIC OZONE OVER CHINA

摘要

An updated version of the Regional Acid Deposition Model(RADM)driven by meteorological fields derived from Chinese Regional Climate Model(CregCM)is used to simulate seasonal variation of troposphertic zone over the eastern China. The results show that: (1) Peak O_3 concentration moves from south China to north China responding to the changing of Solar perpendicular incidence point from south to north.