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OH and HO2 chemistry during NAMBLEX: roles of oxygenates, halogen oxides and heterogenous uptake

By R. Sommariva, William J. Bloss, N. Brough, Nicola Carslaw, M. Flynn, A.-L. Haggerstone, Dwayne E. Heard, James R. Hopkins, James D. Lee, Alastair C. Lewis, Gordon McFiggans, Paul S. Monks, Stuart A. Penkett, Michael J. Pilling, J.M.C. Plane, K.A. Read, A. Saiz-Lopez, Andrew R. Rickard and P.I. Williams

Abstract

This work is licensed under a Creative Commons License and is also available from http://www.copernicus.org/EGU/acp/acp.html, along with any further discussionSeveral zero-dimensional box-models with different levels of chemical complexity, based on the Master Chemical Mechanism (MCM), have been used to study the\ud 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\ud campaign (Mace Head, Ireland) in summer 2002.\ud 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),\ud highlighting their importance for the radical budget. When the models were constrained to measured halogen monoxides (IO, BrO) and used a more detailed,\ud 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\ud monoxides on the modelled concentrations of HOx was dependant on the uptake coefficients used for HOI, HOBr and\ud HO2. Better agreement, within the combined uncertainties of the measurements and of the model, was achieved when using high uptake coefficients for HO2 and HOI (γHO2=1,\ud γHOI=0.6). \ud 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 coreactants for OH and HO2 and of HOX photolysis as a source\ud for OH

Publisher: European Geosciences Union
Year: 2006
OAI identifier: oai:lra.le.ac.uk:2381/121

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