Energy, issue August 2009
This study analyzed the effects of climate and emissions-related perturbations on ozone air quality in Southern California. The future year considered is 2050, with an assumed increase to double pre-industrial levels for global background levels of carbon dioxide. Effects of emission and climate-related forcing on air quality are superimposed on a summer 2005 high-ozone time period. Perturbations considered here include (a) effect of increased temperature on atmospheric reaction rates, (b) effect of increased temperature on biogenic emissions, (c) effect of increased water vapor concentrations, (d) effect of increased pollutant levels at the inflow (western) boundary, and (e) effect of population growth and technology change on emissions within the study domain. Various combinations of the above perturbations are also considered. The climate-related perturbations (a–c) led to combined ozone increases of up to 11 parts per billion for peak one-hour readings, with temperature and humidity effects dominating. The effect on ozone was greatly reduced when the temperature increase was made during nighttime hours rather than uniformly throughout the day. Increased pollutant levels at the inflow boundary also led to ozone increases up to 5 parts per billion. These climate and inflow-related changes offset some of the anticipated benefits of emission controls within the South Coast Air Basin.
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