1Department of Chemistry, University of Leeds, Leeds, UK
2Department of Chemistry, University of York, York, UK
3School of Environmental Sciences, University of East Anglia, Norwich, UK
4Environment Department, University of York, York, UK
5Department of Chemistry, University of Leicester, Leicester, UK
6School of Earth, Atmospheric & Environmental Sciences, University of Manchester, Manchester, UK
*now at: Earth System Research Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
**now at: Department of Chemistry, University of York, York, UK
***now at: Department of Chemistry, University of Leeds, Leeds, UK
Abstract. Several zero-dimensional box-models with different levels of chemical complexity, based on the Master Chemical Mechanism (MCM), have been used to study the chemistry of OH and HO2 in a coastal environment in the Northern Hemisphere. The models were constrained to and compared with measurements made during the NAMBLEX campaign (Mace Head, Ireland) in summer 2002.
The base models, which were constrained to measured CO, CH4 and NMHCs, were able to reproduce [OH] within 25%, but overestimated [HO2] by about a factor of 2. Agreement was improved when the models were constrained to oxygenated compounds (acetaldehyde, methanol and acetone), highlighting their importance for the radical budget. When the models were constrained to measured halogen monoxides (IO, BrO) and used a more detailed, measurements-based, treatment to describe the heterogeneous uptake, modelled [OH] increased by up to 15% and [HO2] decreased by up to 30%. The actual impact of halogen monoxides on the modelled concentrations of HOx was dependant on the uptake coefficients used for HOI, HOBr and HO2. The best agreement with the measurements was achieved by constraining the model to measured IO and setting γHO2=1 and γHOI=0.6.
A rate of production and destruction analysis of the models allowed a detailed study of OH and HO2 chemistry under the conditions encountered during NAMBLEX, showing the importance of oxygenates and of XO (where X=I, Br) as co-reactants for OH and HO2 and of HOX photolysis as a source for OH.