Atmos. Chem. Phys. Discuss., 13, 6923-6969, 2013
www.atmos-chem-phys-discuss.net/13/6923/2013/
doi:10.5194/acpd-13-6923-2013
© Author(s) 2013. 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.
A comparison of atmospheric composition using the Carbon Bond and Regional Atmospheric Chemistry Mechanisms
G. Sarwar1, J. Godowitch1, B. Henderson2, K. Fahey1, G. Pouliot1, W. T. Hutzell1, R. Mathur1, D. Kang3, W. S. Goliff4, and W. R. Stockwell5
1Atmospheric Modeling and Analysis Division, National Exposure Research Laboratory, US Environmental Protection Agency, RTP, NC 27711, USA
2Environmental Engineering Sciences, University of Florida, Gainesville, FL 32611, USA
3Computer Sciences Corporation, RTP, NC 27709, USA
4College of Engineering Center for Environmental Research and Technology, University of California at Riverside, Riverside, CA 92507, USA
5Department of Chemistry, Howard University, Washington, DC 20059, USA

Abstract. We incorporate the recently developed Regional Atmospheric Chemistry Mechanism (version 2, RACM2) into the Community Multiscale Air Quality modeling system for comparison with the existing 2005 Carbon Bond mechanism with updated toluene chemistry (CB05TU). Compared to CB05TU, RACM2 enhances the domain-wide monthly mean hydroxyl radical concentrations by 46% and nitric acid by 26%. However, it reduces hydrogen peroxide by 2%, peroxyacetic acid by 94%, methyl hydrogen peroxide by 19%, peroxyacetyl nitrate by 40%, and organic nitrate by 41%. RACM2 predictions generally agree better with the observed data than the CB05TU predictions. RACM2 enhances ozone for all ambient levels leading to higher bias at low (< 60 ppbv) concentrations but improved performance at high (>70 ppbv) concentrations. The RACM2 ozone predictions are also supported by increased ozone production efficiency that agrees better with observations. Compared to CB05TU, RACM2 enhances the domain-wide monthly mean sulfate by 10%, nitrate by 6%, ammonium by 10%, anthropogenic secondary organic aerosols by 42%, biogenic secondary organic aerosols by 5%, and in-cloud secondary organic aerosols by 7%. Increased inorganic and organic aerosols with RACM2 agree better with observed data. While RACM2 enhances ozone and secondary aerosols by relatively large margins, control strategies developed for ozone or fine particles using the two mechanisms do not differ appreciably.

Citation: Sarwar, G., Godowitch, J., Henderson, B., Fahey, K., Pouliot, G., Hutzell, W. T., Mathur, R., Kang, D., Goliff, W. S., and Stockwell, W. R.: A comparison of atmospheric composition using the Carbon Bond and Regional Atmospheric Chemistry Mechanisms, Atmos. Chem. Phys. Discuss., 13, 6923-6969, doi:10.5194/acpd-13-6923-2013, 2013.
 
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