Photo-oxidant chemistry in the polluted boundary layer under changing UV-B radiation |
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| Affiliation: | 1. State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;2. Chengdu Plain Urban Meteorology and Environment Scientific Observation and Research Station of Sichuan Province, School of Atmospheric Sciences, Chengdu University of Information Technology, Chengdu 610225, China;3. Institute of Nature and Environmental Technology, Kanazawa University, Kakuma–machi, Kanazawa 920–1192, Japan;4. Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science and Technology, Nanjing 210044, China;5. Institute of Arid Meteorology, China Meteorological Administration; Key Laboratory of Arid Climatic Change and Reducing Disaster of Gansu Province; Key Laboratory of Arid Climatic Chance and Disaster Reduction, Lanzhou, Northwestern Regional Center of Numerical Weather Prediction, China;1. Department of Environmental Sciences and Engineering, Xi''an Jiaotong University, Xi''an, China;2. Key Lab of Aerosol, SKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xi''an, China;3. Air Quality Research Division, Environment Canada, Toronto, Canada;4. School of Architecture, Xi''an University of Architecture and Technology, Xi''an 710055, China |
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| Abstract: | UV-B radiation is a driving factor for the chemistry of the polluted boundary layer. It is involved in the formation of radicals and consequently influences the formation and concentration of photo-oxidants. The 3-D mesoscale photochemical Metphomod model was employed to study the effect of changes in UV-B radiation on the concentration of photo-oxidants in the boundary layer over the Swiss Plateau. The model chemistry is based on the RACM mechanism and a two-stream approximation of radiative transfer. A summer (July) and a late winter (February) episode were simulated. All simulations were replicated with relatively large changes in the prescribed total ozone. The results for an increase in UV-B radiation show increases in PAN, HNO3, and ozone at noon in NOx-rich areas and a decrease in NOx. In NOx-poor areas in summer the effect on ozone is weak and has a negative sign, the main effect being an increase in H2O2. The spatial variability of NOx concentrations in the Swiss Plateau in the summer case is such that the effect of increased UV-B radiation on ozone is spatially variable. The effect on the ozone production rate in summer is strongest positive at the surface in the NOx-rich regions in the morning and strongest negative at some altitude above ground in NOx-poor regions in the early afternoon. In the winter episode, NOx-rich conditions are found almost everywhere on the Swiss Plateau, the effect of increased UV-B radiation on the ozone production rate is positive all day long and is largest at 300 m above ground at noon. In this case, in contrast to the summer case, the increase in ozone is carried over to the next day. The model results for ozone are in good agreement with results from a case study and a time series analysis of surface ozone measurements. We estimate the effect of day-to-day changes in total ozone on surface ozone peaks to range from 4 to 6 ppb at most. |
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