Atmos. Chem. Phys. Discuss., 10, 15295-15323, 2010
www.atmos-chem-phys-discuss.net/10/15295/2010/
doi:10.5194/acpd-10-15295-2010
© Author(s) 2010. This work is distributed
under the Creative Commons Attribution 3.0 License.
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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.
Measurements of HONO during BAQS-Met
J. J. B. Wentzell1,2,*, C. L. Schiller1,2,**, and G. W. Harris1,2
1Department of Chemistry, York University, Toronto, Ontario, Canada
2Centre for Atmospheric Chemistry, York University, Toronto, Ontario, Canada
*now at: Environment Canada, Science and Technology Branch, Toronto, ON, Canada
**now at: Environment Canada, Science and Technology Branch, Vancouver, BC, Canada

Abstract. Measurements of nitrous acid (HONO) were performed as part of the 2007 Border Air Quality and Meteorology Study (BAQS-Met) at the Harrow Ontario supersite between 20 June and 10 July 2007. Nitrous acid is an important precursor of the hydroxy radical and understanding its chemistry is important to understanding daytime oxidation chemistry. The HONO measurements were made using a custom built Long Path Absorption Photometer (LOPAP). The goal of this work was to shed light on sources of daytime HONO in the border region. During the course of the campaign HONO mixing ratios consistently exceeded expected daytime values by as much as a factor of 6. Mean daytime concentrations of 61 pptv were observed. While HONO decay began at sunrise, minimum HONO values were not measured until the late afternoon. There was little difference between the daytime (mean=1.5%) and night-time (mean=1.7%) ratios of HONO/NO2. Thus there was a very strong daytime source of HONO which is consistent with other recent studies. Correlations of daytime HONO production with a variety of chemical and meteorological parameters indicate that production is dependent on UV radiation, NO2 and water vapour but is not consistent with a simple gas phase process. Apparent rate constants for the production of HONO from photolyticly excited NO2 and water vapour vary from 2.8–7.8×10−3 molec−1 s−1, during the campaign.

Citation: Wentzell, J. J. B., Schiller, C. L., and Harris, G. W.: Measurements of HONO during BAQS-Met, Atmos. Chem. Phys. Discuss., 10, 15295-15323, doi:10.5194/acpd-10-15295-2010, 2010.
 
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