Publication | Open Access
Hot Summers: Effect of Extreme Temperatures on Ozone in Sydney, Australia
35
Citations
48
References
2018
Year
EngineeringAtmospheric PhotochemistryPoor Air QualityAir QualityClimate ModelingHot SummersEarth ScienceAtmospheric ScienceMicrometeorologyExtreme HeatHot WeatherClimate ChangeOzone Layer DepletionClimate SciencesMeteorologyExtreme TemperaturesAtmospheric HazardOzoneClimatologyMedical MeteorologyAtmospheric ConditionAir Pollution ClimatologyAtmospheric Impact AssessmentAtmospheric TransportAir Pollution
Hot weather is linked to poor air quality, but the precise contribution of high temperatures remains unclear. This study investigates how extreme heat in January 2013 affected ozone levels in Greater Sydney. Using observations from 17 sites and WRF‑Chem, the authors performed sensitivity runs that varied biogenic emissions and temperature treatments to isolate their individual and combined impacts on ozone. The results indicate that temperature‑driven reaction rate changes and biogenic emissions each raise ozone, with combined effects up to 16 ppbv, and that eliminating biogenic emissions removes ozone episodes during heat waves, highlighting their key role.
Poor air quality is often associated with hot weather, but the quantitative attribution of high temperatures on air quality remains unclear. In this study, the effect of elevated temperatures on air quality is investigated in Greater Sydney using January 2013, a period of extreme heat during which temperatures at times exceeded 40 °C, as a case study. Using observations from 17 measurement sites and the Weather Research and Forecasting Chemistry (WRF-Chem) model, we analyse the effect of elevated temperatures on ozone in Sydney by running a number of sensitivity studies in which: (1) the model is run with biogenic emissions generated by MEGAN and separately run with monthly average Model of Emissions of Gases and Aerosols from Nature ( MEGAN) biogenic emissions (for January 2013); (2) the model results from the standard run are compared with those in which average temperatures (for January 2013) are only applied to the chemistry; (3) the model is run using both averaged biogenic emissions and temperatures; and (4 and 5) the model is run with half and zero biogenic emissions. The results show that the impact on simulated ozone through the effect of temperature on reaction rates is similar to the impact via the effect of temperature on biogenic emissions and the relative impacts are largely additive when compared to the run in which both are averaged. When averaged across 17 sites in Greater Sydney, the differences between ozone simulated under standard and averaged model conditions are as high as 16 ppbv. Removing biogenic emissions in the model has the effect of removing all simulated ozone episodes during extreme heat periods, highlighting the important role of biogenic emissions in Australia, where Eucalypts are a key biogenic source.
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