In recent years,ozone(O3)has become the primary pollutant affecting surface air quality in summer in Shijiazhuang.In addition to photochemical generation,surface O3concentrations are also influenced by the physical conditions of the upper atmospheric mixing and vertical boundary layer,and as the height of urban buildings continues to increase,researches on high-altitude pollution are receiving increasing attention.However,the existing studies on O3 pollution in this region were mainly focused on the ground level,and there is a lack of studies on O3 generation at higher altitudes.Therefore,this study analysed the vertical distribution characteristics of O3 and the causes and sources of heavy pollution based on vertical observations of O3 from gradient monitoring stations and ground-based Li DAR,and explored scientific issues such as the factors influencing O3 in the vertical direction,photochemical effects and the evolution of sensitivity using the Generalized Additive Model(GAM),Observation-based Box Model(OBM),combined with methods and tools such as Relative Incremental Reactivity(RIR)and pollutant source analysis models.The analysis showed that the average O3 concentration in the peak season(the highest daily maximum 8-hour average O3 concentration for six consecutive months,May~October)was 1.95 times higher than that in the non-peak season(November~April),and O3 exhibited a positive gradient distribution in the range of 20~200 m in the non-peak season,while the highest O3 concentration was found at 116 m in the peak season.In the height range of0.3~3.0 km during the heavy pollution period in summer(June~August),O3 decreased with increasing altitude in the range of 0.3~3.0 km,and showed positive gradient distribution characteristics in 0.37~0.76 km,and the O3 concentration was most stable and highest in the 0.76~1.16 km,after which the O3 concentration decreased in a wave-like manner with increasing height.Correlation analysis showed that the meteorological factors with the highest correlation with O3 were temperature and UVB in peak and non-peak seasons,respectively,and among the pollutant factors,NO and NO2 were significantly negatively correlated with O3.The GAM results also showed that NO was a major influencing factor for O3 variation throughout the year,and the most important meteorological factors for the peak and non-peak seasons of O3 were temperature and UVB,respectively.Simulation results based on the OBM model indicated that strong photochemical reactions were an important driver for O3 pollution and atmospheric photochemistry was more important for the surface O3.Through the calculation of RIR,it was determined that alkenes were the precursors with the greatest impact on O3,and among typical species,isoprene and ethylene have the highest RIR values in the peak and non-peak seasons,respectively,indicating the influence of plant emissions and traffic emissions.In simulations of different pollution scenarios,it was found that increasing NO concentrations favoured O3pollution mitigation,and the abundance of·OH was a significant feature of O3photochemical reactions and dominated the effect of changes in NO concentration on O3.The analysis of the causes of heavy O3 pollution showed that local photochemical generation combined with vertical transport was an important reason for heavy O3 pollution,and the pollution trajectory that had a greater impact on the ground came from the local area of Shijiazhuang,with the contribution of urban areas to O3 concentration in Shijiazhuang exceeding 70μg·m-3 at different heights,while external transport sources including Xingtai,Handan,Cangzhou in Hebei province and Yangquan in Shanxi province. |