Air quality study of high ozone levels in South California Amela Jeričević1, Darko Koračin2, Jinhua Jiang2, Judith Chow2, John Watson2, Eric Fujita2 and Hiroaki Minoura3 1 Croatian Meteorological and Hydrological Service, Gric 3, 10000 Zgreb, Croatia. 2 Desert Research Institute, University and Community College System of Nevada, P.O. Box 60220, Reno, NV 89506, U.S.A. 3 Toyota Motor Engineering & Manufacturing North America, Inc., 1555 Woodridge Ave, Ann Arbor, MI 4810, U.S.A. Abstract Physical and chemical characteristics within the two distinct meteorological regimes, i.e., convective and stable atmospheric conditions in a complex highly urbanized terrain of the California South Coast Air Basin (CSCAB; the Los Angeles area) were investigated. The Community Multiscale Air Quality (CMAQ) model was used with a horizontal resolution of 5 km x 5 km to produce the 3D fields of pollutant concentrations. Input meteorological fields were obtained by the MM5 numerical weather prediction model while the input emissions were provided by the Californian Environmental Protection Agency. Modeled meteorological surface parameters and their vertical profiles as well as modeled planetary boundary layer heights (PBL) were compared to the corresponding measurements. The CMAQ simulations of ozone concentrations were compared against the relatively large number of measurements from the CSCAB area. The main goal of the research was to identify the governing atmospheric processes and sources in the coastal area that contributed to the high levels of pollution and to investigate the air quality model's capabilities to simulate the air quality in the complex topography. Introduction The California South Coast Air Basin (CSCAB; the Los Angeles area) is known for its air pollution problems, especially for photochemical smog episodes. There has been a considerable amount of studies of air pollution 2 in California (e.g., Blumenthal et al. 1977; Farber et al., 1982; Roth et al., 1984; Luria et a. 2005). Frequently observed high levels of pollutants occur due to elevated anthropogenic emissions as well as due to special air circulation patterns which drive the pollutants complex temporal and spatial distribution. In this work an episode of high ozone concentrations that occurred in July 2005 was analyzed. CMAQ model was applied in order to investigate spatial and temporal distribution of pollutants and advantages and limitations as well as recommendations for future work are presented in this paper. Results Ozone observations in California South Coast Air Basin Measured hourly ozone concentrations from 21 stations in the domain during July 2005 are used for investigation. Due to specific meteorological conditions spatial and temporal distributions in surface ozone concentrations were not uniform especially during the episode of high ozone concentrations between 15 and 20 July 2005. Areas with different observed ozone levels were identified. Daily distributions of measured and modeled hourly ozone and NO2 concentrations at different stations in CSCAB domain during July 2005 are shown in Fig.1.Generally the highest ozone concentrations are observed on the stations inland in the eastern part of the Los Angeles (e.g., station 2077 in Fig. 1.) while the lowest levels are present at coastal stations on the west part (e.g., station 2937 in Fig. 1.). Medium levels with characteristic urban patterns are visible on 4 stations situated in the domain centre (e.g., station 2898 and 2160 in Fig. 1.). For most of the stations measured ozone concentrations are characteristic for urban areas being the highest during the daytime when chemical production of ozone occurs in presence of NOx and sunlight and low nighttime ozone levels resulting from titration with NOx. The ozone July episode was most intensive in the inland stations on the eastern part of the Los Angeles while at coastal stations on the west part ozone levels were low and without high daily variations. 3 2077 2898 20 20 15 15 10 10 5 5 ppm 0.135 0.12 0.105 0 5 10 15 20 25 30 0 5 10 2160 15 20 25 30 2937 20 20 15 15 10 10 5 5 0.09 0.075 0.06 0.045 0.03 0.015 0 0 5 10 15 20 25 30 0 5 10 15 20 25 30 Figure 1. Daily distribution of measured hourly ozone concentrations at different stations in CSCAB (California South Coast Air Basin) domain during July 2005. CMAQ simulations Surface high pressure system with subsiding air resulting in stable atmospheric conditions was present over the sea and in the coastal area while low pressure areas in the central and eastern part of the domain, where high ozone concentrations were measured, was prevailing during the episode (not shown). Surface wind speeds were generally low, especially during the night, with prevailing west direction. Modeled planetary boundary layer heights (PBL) were uniformly low during the nighttime while during the daytime in the southwest and central part of the domain low PBL values were present and northeast and east parts of the domain had significantly higher PBL values (not shown). Areas with higher daytime PBL hight corresponds to the low pressure systems and high measured ozone levels were characterized with unstable, turbulent processes and intensive and mixing in the atmosphere. 4 Intercomparison of the measured hourly ozone concentrations to the modeled ozone and NO2 values for different stations in the CSCAB (California South Coast Air Basin) domain are shown in Fig. 2. Generally model underestimates measured ozone values but model showed an ability to reproduce daily variations and high correlation factors ~ 0.7 are found for most of the stations. Also boundary conditions used in CMAQ simulations were provided using profile option. However, a test with different boundary conditions (not shown) using the nesting option into a lower resolution CMAQ run on the larger domain showed a much better agreement with the measurements indicating that significant contribution to the high ozone levels was originating from the larger Californian area . Conclusions An application of CMAQ air pollution model was conducted on an ozone episode occurred in July 2005. It is found that model was able to reproduce complex physical and chemical phenomena within the two distinct meteorological regimes, i.e., convective and stable atmospheric conditions in a complex highly urbanized terrain of the California South Coast Air Basin (CSCAB; the Los Angeles area). Due to the fact that the highest ozone levels were found to be related with unstable conditions and high mixing in further work special attention should be given to the investigation of the relationship between the pollutant concentrations and turbulence characteristics in PBL including the investigation of existing vertical diffusion schemes performance in the CMAQ model. References Blumenthal D.L., White, W.H. and T.B. Smith, 1977.:’Anatomy of a Los Angeles smog episode: Pollutant transport in the daytime sea breeze regime’, Atm. Environ. Vol. 12, pp. 893-907. Farber R.J., Huang, A.A., Bregman, L.D., Mahoney R.L., Eatough D.J., Hansen L.D., Blumenthal D.L., Keifer, W.S. and D.W. Allard, 1982.:’The third in the Los Angeles Basin’, The Sci. of the total Environ. 23, 345-360. Roth, P.M., Reynolds, S.D., Tesche, T.W., Gutfreund, P.D. and C. Seigneur:’An appraisal of emissions control requirements in the California South Coast Air Basin’, Environ. Int., Vol. 9, 549-571. Luria, M., tanner, R.L., Valente, R.J., Bairai, S.T., Koracin, D. and A.W. Gertler, 2005.:’Local and transported pollution over San Diego, California’, Atm. Environ., Vol. 39, 6765-6776. 5 0.18 2898 Pomona 0.16 concentrations 0.14 0.12 0.1 0.08 0.06 0.04 0.02 0 0 6 12 18 24 30 36 42 48 54 60 66 72 78 84 90 96 hours 0.18 0.18 2937 Costa Mesa 0.16 0.08 ozone_obs concentrations ozone_model -0.02 0.14 0612 18 23436 0448 256466 072 78 890 496 0.12 NO2_model 0.1 NO2_obs 0.08 0.06 0.04 0.02 0 0 6 12 18 24 30 36 42 48 54 60 66 72 78 84 90 96 hours Figure 2. Daily course of measured hourly ozone concentrations (column) and NO2 (black dot) values and modeled ozone (thick black line) and NO2 (thin black line) values on different stations in the CSCAB (California South Coast Air Basin) domain during 15 and 16 July 2005.