| Autor: |
Sherwen T; Wolfson Atmospheric Chemistry Laboratory, University of York, York, UK. tomas.sherwen@york.ac.uk., Evans MJ; Wolfson Atmospheric Chemistry Laboratory, University of York, York, UK. tomas.sherwen@york.ac.uk and National Centre for Atmospheric Science (NCAS), University of York, York, UK., Sommariva R; Department of Chemistry, University of Leicester, Leicester, UK., Hollis LDJ; Department of Chemistry, University of Leicester, Leicester, UK., Ball SM; Department of Chemistry, University of Leicester, Leicester, UK., Monks PS; Department of Chemistry, University of Leicester, Leicester, UK., Reed C; Wolfson Atmospheric Chemistry Laboratory, University of York, York, UK. tomas.sherwen@york.ac.uk., Carpenter LJ; Wolfson Atmospheric Chemistry Laboratory, University of York, York, UK. tomas.sherwen@york.ac.uk., Lee JD; Wolfson Atmospheric Chemistry Laboratory, University of York, York, UK. tomas.sherwen@york.ac.uk and National Centre for Atmospheric Science (NCAS), University of York, York, UK., Forster G; NCAS, School of Environmental Sciences, University of East Anglia, Norwich, UK and School of Environmental Sciences, University of East Anglia, Norwich, UK., Bandy B; School of Environmental Sciences, University of East Anglia, Norwich, UK., Reeves CE; School of Environmental Sciences, University of East Anglia, Norwich, UK., Bloss WJ; School of Geography, Earth and Environmental Science, University of Birmingham, Birmingham, UK. |
| Abstrakt: |
Halogens (Cl, Br) have a profound influence on stratospheric ozone (O 3 ). They (Cl, Br and I) have recently also been shown to impact the troposphere, notably by reducing the mixing ratios of O 3 and OH. Their potential for impacting regional air-quality is less well understood. We explore the impact of halogens on regional pollutants (focussing on O 3 ) with the European grid of the GEOS-Chem model (0.25° × 0.3125°). It has recently been updated to include a representation of halogen chemistry. We focus on the summer of 2015 during the ICOZA campaign at the Weybourne Atmospheric Observatory on the North Sea coast of the UK. Comparisons between these observations together with those from the UK air-quality network show that the model has some skill in representing the mixing ratios/concentration of pollutants during this period. Although the model has some success in simulating the Weybourne ClNO 2 observations, it significantly underestimates ClNO 2 observations reported at inland locations. It also underestimates mixing ratios of IO, OIO, I 2 and BrO, but this may reflect the coastal nature of these observations. Model simulations, with and without halogens, highlight the processes by which halogens can impact O 3 . Throughout the domain O 3 mixing ratios are reduced by halogens. In northern Europe this is due to a change in the background O 3 advected into the region, whereas in southern Europe this is due to local chemistry driven by Mediterranean emissions. The proportion of hourly O 3 above 50 nmol mol -1 in Europe is reduced from 46% to 18% by halogens. ClNO 2 from N 2 O 5 uptake onto sea-salt leads to increases in O 3 mixing ratio, but these are smaller than the decreases caused by the bromine and iodine. 12% of ethane and 16% of acetone within the boundary layer is oxidised by Cl. Aerosol response to halogens is complex with small (∼10%) reductions in PM 2.5 in most locations. A lack of observational constraints coupled to large uncertainties in emissions and chemical processing of halogens make these conclusions tentative at best. However, the results here point to the potential for halogen chemistry to influence air quality policy in Europe and other parts of the world. |
