Atmos. Chem. Phys. Discuss., 10, 4143-4188, 2010
www.atmos-chem-phys-discuss.net/10/4143/2010/
doi:10.5194/acpd-10-4143-2010
© Author(s) 2010. This work is distributed
under the Creative Commons Attribution 3.0 License.
Review Status
This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Impacts of HONO sources on the photochemistry in Mexico City during the MCMA-2006/MILAGO Campaign
G. Li1,2, W. Lei1,2, M. Zavala1, R. Volkamer3,4, S. Dusanter5, P. Stevens5, and L. T. Molina1,2
1Molina Center for the Energy and the Environment, La Jolla, CA 92037, USA
2Massachusetts Institute of Technology, Cambridge, MA 02139, USA
3Department of Chemistry, University of Colorado at Boulder, 215 UCB, Boulder, CO 80309, USA
4Cooperative Institute for Research in the Environmental Sciences (CIRES), University of Colorado at Boulder, 216 UCB, Boulder, CO 80309, USA
5Center for Research in Environmental Science, School of Public and Environmental Affairs, and Department of Chemistry, Indiana University, Bloomington, IN 47405, USA

Abstract. The contribution of HONO sources to the photochemistry in Mexico City is investigated during the MCMA-2006/MILAGO Campaign using the WRF-CHEM model. Besides the homogeneous reaction of NO with OH, four additional HONO sources are considered in the WRF-CHEM model: secondary HONO formation from NO2 heterogeneous reaction with semivolatile organics, NO2 reaction with freshly emitted soot, NO2 heterogeneous reaction on aerosol and ground surfaces. The WRF-CHEM model with the five HONO sources performs reasonably well in tracking the observed diurnal variation of HONO concentrations. The HONO sources included are found to significantly improve the HOx (OH+HO2) simulations during daytime and the partition of NO/NO2 in the morning. The HONO sources also accelerate the accumulation of O3 concentrations in the morning by about 2 h and subsequently result in a noticeable enhancement of O3 concentrations over the course of the day with a midday average of about 6 ppb. Furthermore, these HONO sources play a very important role in the formation of secondary aerosols in the morning. They substantially enhance the secondary organic aerosol concentrations by a factor of 2 on average in the morning, although contribute less during the rest of the day. The simulated nitrate and ammonium aerosols are also remarkably enhanced in the morning when the four HONO sources are added, in good agreement with the measurements. The impact of the HONO sources on the sulfate aerosols is negligible because of the inefficient conversion of H2SO4 from SO2 reacting with OH.

Citation: Li, G., Lei, W., Zavala, M., Volkamer, R., Dusanter, S., Stevens, P., and Molina, L. T.: Impacts of HONO sources on the photochemistry in Mexico City during the MCMA-2006/MILAGO Campaign, Atmos. Chem. Phys. Discuss., 10, 4143-4188, doi:10.5194/acpd-10-4143-2010, 2010.
 
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