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Volume 11, issue 8 | Copyright

Special issue: Megacities: air quality and climate impacts from local to...

Atmos. Chem. Phys., 11, 3847-3864, 2011
https://doi.org/10.5194/acp-11-3847-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 27 Apr 2011

Research article | 27 Apr 2011

The impact of temperature changes on summer time ozone and its precursors in the Eastern Mediterranean

U. Im1, K. Markakis2, A. Poupkou2, D. Melas2, A. Unal3, E. Gerasopoulos4, N. Daskalakis1, T. Kindap3, and M. Kanakidou1 U. Im et al.
  • 1Environmental Chemical Processes Laboratory (ECPL), Department of Chemistry, University of Crete, Heraklion, Greece
  • 2Aristotle University of Thessaloniki, Department of Physics, Laboratory of Atmospheric Physics, Thessaloniki, Greece
  • 3Istanbul Technical University, Eurasia Institute of Earth Sciences, Istanbul, Turkey
  • 4Institute for Environmental Research and Sustainable Development, National Observatory of Athens, Athens, Greece

Abstract. Changes in temperature due to variability in meteorology and climate change are expected to significantly impact atmospheric composition. The Mediterranean is a climate sensitive region and includes megacities like Istanbul and large urban agglomerations such as Athens. The effect of temperature changes on gaseous air pollutant levels and the atmospheric processes that are controlling them in the Eastern Mediterranean are here investigated. The WRF/CMAQ mesoscale modeling system is used, coupled with the MEGAN model for the processing of biogenic volatile organic compound emissions. A set of temperature perturbations (spanning from 1 to 5 K) is applied on a base case simulation corresponding to July 2004. The results indicate that the Eastern Mediterranean basin acts as a reservoir of pollutants and their precursor emissions from large urban agglomerations. During summer, chemistry is a major sink at these urban areas near the surface, and a minor contributor at downwind areas. On average, the atmospheric processes are more effective within the first 1000 m above ground. Temperature increases lead to increases in biogenic emissions by 9±3% K−1. Ozone mixing ratios increase almost linearly with the increases in ambient temperatures by 1±0.1 ppb O3 K−1 for all studied urban and receptor stations except for Istanbul, where a 0.4±0.1 ppb O3 K−1 increase is calculated, which is about half of the domain-averaged increase of 0.9±0.1 ppb O3 K−1. The computed changes in atmospheric processes are also linearly related with temperature changes.

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