Abstract

Abstract. In this study, WRF-Chem is utilized at high resolution (1.333 km grid spacing for the innermost domain) to investigate impacts of southern California anthropogenic emissions (SoCal) on Phoenix ground-level ozone concentrations ([O3]) for a pair of recent exceedance episodes. First, WRF-Chem control simulations, based on the US Environmental Protection Agency (EPA) 2005 National Emissions Inventories (NEI05), are conducted to evaluate model performance. Compared with surface observations of hourly ozone, CO, NOX, and wind fields, the control simulations reproduce observed variability well. Simulated [O3] are comparable with the previous studies in this region. Next, the relative contribution of SoCal and Arizona local anthropogenic emissions (AZ) to ozone exceedances within the Phoenix metropolitan area is investigated via a trio of sensitivity simulations: (1) SoCal emissions are excluded, with all other emissions as in Control; (2) AZ emissions are excluded with all other emissions as in Control; and (3) SoCal and AZ emissions are excluded (i.e., all anthropogenic emissions are eliminated) to account only for Biogenic emissions and lateral boundary inflow (BILB). Based on the USEPA NEI05, results for the selected events indicate the impacts of AZ emissions are dominant on daily maximum 8 h average (DMA8) [O3] in Phoenix. SoCal contributions to DMA8 [O3] for the Phoenix metropolitan area range from a few ppbv to over 30 ppbv (10–30 % relative to Control experiments). [O3] from SoCal and AZ emissions exhibit the expected diurnal characteristics that are determined by physical and photochemical processes, while BILB contributions to DMA8 [O3] in Phoenix also play a key role. Finally, ozone transport processes and pathways within the lower troposphere are investigated. During daytime, pollutants (mainly ozone) near the Southern California coasts are pumped into the planetary boundary-layer over the Southern California desert through the mountain chimney and pass channel effects, aiding eastward transport along the desert air basins in southern California and finally, northeastward along the lower Gila River basin in Arizona, thereby affecting Phoenix air quality during subsequent days. This study indicates that local emission controls in Phoenix need to be augmented with regional emission reductions to attain the federal ozone standard, especially if a more stringent standard is adopted in the future.

Highlights

  • Tropospheric ozone is a strong oxidant controlling much of the chemistry in the atmosphere, such as hydroxyl radical production and the lifetime of atmospheric species

  • Model simulations have been compared with surface observations of hourly ozone, CO, NOX and wind fields in Southern California and Arizona

  • The results indicate that the Weather Research and Forecasting (WRF)-Chem configuration in this study can adequately simulate the spatial distribution, the magnitude, and the variability of the observations

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Summary

Introduction

Tropospheric ozone is a strong oxidant controlling much of the chemistry in the atmosphere, such as hydroxyl radical production and the lifetime of atmospheric species (see review in He et al, 2013). Tropospheric ozone is a greenhouse gas and acts as an important anthropogenic contributor to radiative forcing of climate (IPCC, 2007). Lower tropospheric ozone adversely affects human health (Anderson, 2009; Smith et al, 2009), reduces crop yields (Avnery et al, 2011; Chameides et al, 1999), and damages natural ecosystems (Ashmore, 2005; Mauzerall and Wang, 2001). Ozone (O3) is one of the six criteria pollutants regulated by the US Environmental Protection Agency (EPA) through National Ambient Air Quality Standards (NAAQS).

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