Atmos. Chem. Phys. Discuss., 4, 419-470, 2004
www.atmos-chem-phys-discuss.net/4/419/2004/
doi:10.5194/acpd-4-419-2004
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This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
OH and HO2 chemistry in clean marine air during SOAPEX-2
R. Sommariva1, A.-L. Haggerstone2, L. J. Carpenter2, N. Carslaw3, D. J. Creasey1,*, D. E. Heard1, J. D. Lee1,**, A. C. Lewis1,**, M. J. Pilling1, and J. Zádor4
1Department of Chemistry, University of Leeds, Leeds, UK
2Department of Chemistry, University of York, York, UK
3Environment Department, University of York, York, UK
4Department of Physical Chemistry, Eötvös University (ELTE), Budapest, Hungary
*Now at Photonic Solutions plc., Gracemount Business Pavilions Unit A2/A3, 40 Captains Rd., Edinburgh, UK
**Now at Department of Chemistry, University of York, York, UK

Abstract. Model-measurement comparisons of HOx in extremely clean air ([NO]<3  ppt) are reported. Measurements were made during the second Southern Ocean Photochemistry Experiment (SOAPEX-2), held in austral summer 1999 at the Cape Grim Baseline Air Pollution Station in north-western Tasmania, Australia.

The free-radical chemistry was studied using a zero-dimensional box-model based upon the Master Chemical Mechanism (MCM). Two versions of the model were used, with different levels of chemical complexity, to explore the role of hydrocarbons upon free-radical budgets under very clean conditions. The "detailed" model was constrained to measurements of CO, CH4 and 15 NMHCs, while the "simple" model contained only the CO and  CH4 oxidation mechanisms, together with inorganic chemistry. The OH and HO2 (HOx) concentrations predicted by the two models agreed to within 5–10%.

The model results were compared with the HOx concentrations measured by the FAGE (Fluorescence Assay by Gas Expansion) technique during four days of clean Southern Ocean marine boundary layer (MBL) air. The models overestimated OH concentrations by about 10% on two days and about 20% on the other two days. HO2 concentrations were measured during two of these days and the models overestimated the measured concentrations by about 40%. Better agreement with measured HO2 was observed by using data from several MBL aerosol measurements to estimate the aerosol surface area and by increasing the HO2 uptake coefficient to unity. This reduced the modelled HO2 overestimate by ~40%, with little effect on OH, because of the poor HO2 to OH conversion at the low ambient NOx concentrations.

Local sensitivity analysis and Morris One-At-A-Time analysis were performed on the "simple" model, and showed the importance of reliable measurements of j(O1D) and [HCHO] and of the kinetic parameters that determine the efficiency of  O(1D) to OH and HCHO to HO2 conversion. A 2σ standard deviation of 30–40% for OH and 25–30% for HO2 was estimated for the model calculations using a Monte Carlo technique coupled with Latin Hypercube Sampling (LHS).

A rate of production analysis, which demonstrates the relevance of  HCHO as a radical source, coupled with the poor performance of the models with respect to the concentrations of formaldehyde and peroxides, suggest that there are significant uncertainties in the chemical mechanism.


Citation: Sommariva, R., Haggerstone, A.-L., Carpenter, L. J., Carslaw, N., Creasey, D. J., Heard, D. E., Lee, J. D., Lewis, A. C., Pilling, M. J., and Zádor, J.: OH and HO2 chemistry in clean marine air during SOAPEX-2, Atmos. Chem. Phys. Discuss., 4, 419-470, doi:10.5194/acpd-4-419-2004, 2004.
 
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