By means of a three-dimensional meteorological model(MM5)and a chemical model,the distributions of tropospheric ozone and its precursors over China have been simulated in summer and winter time,16—18 August 1994 and ...By means of a three-dimensional meteorological model(MM5)and a chemical model,the distributions of tropospheric ozone and its precursors over China have been simulated in summer and winter time,16—18 August 1994 and 7—9 January 1995.The distribution of ozone over the Tibetan Plateau in summer time is deeply discussed.The simulated results indicate that the distributions of surface ozone and NO_x are in good agreement with observed results,and human activities and photochemical reactions are the main factors controlling the surface ozone and NO_x concentrations.In addition,higher ozone concentrations are coincided with the air convergence, and the lower concentrations are related to the air divergence.In summer,over the Tibetan Plateau the strong flow convergence results in higher ozone concentrations in the lower troposphere:and the strong flow divergence results in lower ozone concentrations in the upper troposphere.In winter time ozone concentrations show Iarge-scale characteristics controlled by westerly flow,and in the jet area they are lower than those outside the jet.展开更多
基金National Natural Science Foundation of China under Grant 49392200.
文摘By means of a three-dimensional meteorological model(MM5)and a chemical model,the distributions of tropospheric ozone and its precursors over China have been simulated in summer and winter time,16—18 August 1994 and 7—9 January 1995.The distribution of ozone over the Tibetan Plateau in summer time is deeply discussed.The simulated results indicate that the distributions of surface ozone and NO_x are in good agreement with observed results,and human activities and photochemical reactions are the main factors controlling the surface ozone and NO_x concentrations.In addition,higher ozone concentrations are coincided with the air convergence, and the lower concentrations are related to the air divergence.In summer,over the Tibetan Plateau the strong flow convergence results in higher ozone concentrations in the lower troposphere:and the strong flow divergence results in lower ozone concentrations in the upper troposphere.In winter time ozone concentrations show Iarge-scale characteristics controlled by westerly flow,and in the jet area they are lower than those outside the jet.
