Atmospheric Chemistry and Physics www.atmos-chem-phys.net 1680-7316 1680-7324 1 1 2001 10.5194/acp-1-9-2001 http://www.atmos-chem-phys.net/1/9/2001/ http://www.atmos-chem-phys.net/1/9/2001/acp-1-9-2001.html http://www.atmos-chem-phys.net/1/9/2001/acp-1-9-2001.pdf 9 18 2001-11-23 Coastal zone production of IO precursors: a 2-dimensional study L. J. Carpenter K. Hebestreit U. Platt P. S. Liss Department of Chemistry, University of York, York, YO10 5DD, UK Institut f¨ur Umweltphysik, University of Heidelberg, INF 229, D-69120 Heidelberg, Germany School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, UK At Mace Head, Eire, in the coastal East Atlantic, diiodomethane has been identified as an important precursor of iodine oxide radicals. Peak concentrations of both CH₂I₂ and IO at low water indicate that the intertidal region is a strong source of organo-iodines. Atmospheric measurements of CH₂I₂ made in marine air are compared with the concentrations predicted by a 2-dimensional model incorporating horizontal and vertical dispersion of surface emissions. The model shows that micrometeorological variability, proximity of the site to emissions, and photolysis all play important roles in determining the CH₂I₂ concentrations at Mace Head. In addition to a tidal-height dependent intertidal flux, which was estimated from seaweed production data, a contribution from offshore (non-local) sources was required in order to reproduce the strong signature of photolysis in the CH₂I₂ observations. A combination of an offshore flux and an intertidal flux (of up to 1.4 × 10⁹ molecules cm^-2s^-1 at low water) results in good agreement between the measured and modelled CH₂I₂ concentrations. Although this study does not necessarily infer emission of CH₂I₂ from the open ocean, it suggests that air-sea exchange of CH₂I₂ in coastal waters does occur.