Articles | Volume 14, issue 14
Atmos. Chem. Phys., 14, 7601–7616, 2014
https://doi.org/10.5194/acp-14-7601-2014
Atmos. Chem. Phys., 14, 7601–7616, 2014
https://doi.org/10.5194/acp-14-7601-2014

Research article 29 Jul 2014

Research article | 29 Jul 2014

The fate of NOx emissions due to nocturnal oxidation at high latitudes: 1-D simulations and sensitivity experiments

P. L. Joyce2,1, R. von Glasow3, and W. R. Simpson2,1 P. L. Joyce et al.
  • 1Department of Chemistry and Biochemistry, University of Alaska, Fairbanks, AK, USA
  • 2Geophysical Institute, University of Alaska, Fairbanks, AK, USA
  • 3Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, University of East Anglia, Norwich, UK

Abstract. The fate of nitrogen oxide pollution during high-latitude winter is controlled by reactions of dinitrogen pentoxide (N2O5) and is highly affected by the competition between heterogeneous atmospheric reactions and deposition to the snowpack. MISTRA (MIcrophysical STRAtus), a 1-D photochemical model, simulated an urban pollution plume from Fairbanks, Alaska to investigate this competition of N2O5 reactions and explore sensitivity to model parameters. It was found that dry deposition of N2O5 made up a significant fraction of N2O5 loss near the snowpack, but reactions on aerosol particles dominated loss of N2O5 over the integrated atmospheric column. Sensitivity experiments found the fate of NOx emissions were most sensitive to NO emission flux, photolysis rates, and ambient temperature. The results indicate a strong sensitivity to urban area density, season and clouds, and temperature, implying a strong sensitivity of the results to urban planning and climate change. Results suggest that secondary formation of particulate (PM2.5) nitrate in the Fairbanks downtown area does not contribute significant mass to the total PM2.5 concentration, but appreciable amounts are formed downwind of downtown due to nocturnal NOx oxidation and subsequent reaction with ammonia on aerosol particles.

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