Summer 2015 measurements of total OH reactivity at a UK coastal site

Abstract:

The hydroxyl radical (OH) plays a central role in the day time oxidative removal of pollutants and greenhouse gases in the atmosphere. It is essential that all production and loss pathways of OH are understood and included in computer models in order to accurately predict OH concentrations for a range of environments, and in turn the rate of production of secondary products, for example ozone and organic aerosol. Direct measurement of total OH reactivity, the pseudo first order rate coefficient for OH loss by reaction with its sinks, is a very useful tool to test how complete our knowledge is of OH loss pathways. Comparison with values of total OH reactivity calculated by computer models using concentrations of simultaneously measured OH ‘sinks’ and unmeasured intermediates enables environments to be identified where there are unidentified ‘missing’ OH sinks. Total OH reactivity was measured using the laser flash photolysis combined with time-resolved laser-induced fluorescence technique during the ICOZA (Integrated Chemistry of OZone in the Atmosphere) campaign in July 2015 at the Weybourne Atmospheric Observatory (WAO), Norfolk, UK. Air masses sampled ranged from polluted air from the UK or Europe containing processed urban emissions to very clean air of marine origin. Data for measured and calculated OH reactivity will be presented in addition to a discussion of the magnitude of the ‘missing’ OH sink determined for each type of air mass.