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AGU: Geophysical Research Letters

 

Index Terms

  • Atmospheric Composition and Structure: Air/sea constituent fluxes
  • Atmospheric Composition and Structure: Geochemical cycles
  • Atmospheric Composition and Structure: Troposphere: composition and chemistry

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 32, L06814, 4 PP., 2005
doi:10.1029/2004GL022084

Impact of halogen monoxide chemistry upon boundary layer OH and HO2 concentrations at a coastal site

W. J. Bloss

Department of Chemistry, University of Leeds, Leeds, UK

J. D. Lee

Department of Chemistry, University of Leeds, Leeds, UK

G. P. Johnson

Department of Chemistry, University of Leeds, Leeds, UK

R. Sommariva

Department of Chemistry, University of Leeds, Leeds, UK

D. E. Heard

Department of Chemistry, University of Leeds, Leeds, UK

A. Saiz-Lopez

School of Environmental Science, University of East Anglia, Norwich, UK

J. M. C. Plane

School of Environmental Science, University of East Anglia, Norwich, UK

G. McFiggans

Physics Department, Institute of Science and Technology, University of Manchester, Manchester, UK

H. Coe

Physics Department, Institute of Science and Technology, University of Manchester, Manchester, UK

M. Flynn

Physics Department, Institute of Science and Technology, University of Manchester, Manchester, UK

P. Williams

Physics Department, Institute of Science and Technology, University of Manchester, Manchester, UK

A. R. Rickard

Department of Chemistry, University of Leicester, Leicester, UK

Z. L. Fleming

Department of Chemistry, University of Leicester, Leicester, UK

The impact of iodine oxide chemistry upon OH and HO2 concentrations in the coastal marine boundary layer has been evaluated using data from the NAMBLEX (North Atlantic Marine Boundary Layer Experiment) campaign, conducted at Mace Head, Ireland during the summer of 2002. Observationally constrained calculations show that under low NOx conditions experienced during NAMBLEX (NO ≤ 50 pptv), the reaction IO + HO2 → HOI + O2 accounted for up to 40% of the total HO2 radical sink, and the subsequent photolysis of HOI to form OH + I comprised up to 15% of the total midday OH production rate. The XO + HO2 (X = Br, I) reactions may in part account for model overestimates of measured HO2 concentrations in previous studies at Mace Head, and should be considered in model studies of HOx chemistry at similar coastal locations.

Received 25 November 2004; accepted 8 March 2005; published 30 March 2005.

Citation: Bloss, W. J., et al. (2005), Impact of halogen monoxide chemistry upon boundary layer OH and HO2 concentrations at a coastal site, Geophys. Res. Lett., 32, L06814, doi:10.1029/2004GL022084.

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