ACP

Atmospheric Chemistry and Physics

ACP

1680-7324

Copernicus GmbH

Göttingen, Germany

10.5194/acp-4-839-2004

OH and HO2 chemistry in clean marine air during SOAPEX-2

Sommariva

¹ Haggerstone

A.-L.

² Carpenter

L. J.

² Carslaw

³ Creasey

D. J.

¹ ⁵ Heard

D. E.

¹ Lee

J. D.

¹ ⁶ Lewis

A. C.

¹ ⁶ Pilling

M. J.

¹ Zádor

⁴

Department of Chemistry, University of Leeds, Leeds, UK

Department of Chemistry, University of York, York, UK

Environment Department, University of York, York, UK

Department of Physical Chemistry, Ëotvös 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

14 06 2004

4 3 839 856

This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

This article is available from http://www.atmos-chem-phys.net/4/839/2004/acp-4-839-2004.html

The full text article is available as a PDF file from http://www.atmos-chem-phys.net/4/839/2004/acp-4-839-2004.pdf

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 17 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).