Atmos. Chem. Phys. Discuss., 10, 20125-20165, 2010
www.atmos-chem-phys-discuss.net/10/20125/2010/
doi:10.5194/acpd-10-20125-2010
© 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.
Evaluation of simulated photochemical partitioning of oxidized nitrogen in the upper troposphere
B. H. Henderson1,2, R. W. Pinder2, J. Crooks2, R. C. Cohen3, W. T. Hutzell2, G. Sarwar2, W. S. Goliff4, W. R. Stockwell5, A. Fahr5, R. Mathur2, A. G. Carlton2, and W. Vizuete1
1Department of Environmental Science and Engineering, University of North Carolina, Chapel Hill, NC, USA
2National Exposure Research Laboratory, US Environmental Protection Agency (USEPA), RTP, NC, USA
3Departments of Chemistry and Earth and Planetary Sciences, University of California, Berkeley, CA, USA
4College of Engineering-CERT, University of California at Riverside, Riverside, CA, USA
5Department of Chemistry, Howard University, Washington, DC, USA

Abstract. Regional and global chemical transport models underpredict NOx (NO+NO2) in the upper troposphere where it is a precursor to the greenhouse gas ozone. The NOx bias been shown in model evaluations using aircraft data (Singh et al., 2007) and total column NO2 (molecules cm−2) from satellite observations (Napelenok et al., 2008). The causes of NOx underpredictions have yet to be fully understood due to the interconnected nature of simulated emission, transport, and chemistry processes. Recent observation-based studies suggest that, in the upper troposphere, simulated chemistry overpredicts hydrogen radicals (OH and HO2) and would convert NOx to HNO3 too quickly (Olson et al., 2006; Bertram et al., 2007; Ren et al., 2008). Since typical chemistry evaluation techniques are not available for upper tropospheric conditions, this study develops an evaluation platform from in situ observations, stochastic convection, and deterministic chemistry. We derive a stochastic convection model and optimize it using two simulated datasets of time since convection, one based on meteorology and the other on chemistry. The chemistry surrogate for time since convection is calculated using seven different chemical mechanisms, all of which predict shorter time since convection than our meteorological analysis. We evaluate chemical simulations by inter-comparison and by pairing results with observations based on NOx:HNO3, a photochemical aging indicator. Inter-comparison reveals individual chemical mechanism biases and recommended updates. Evaluation against observations shows that all chemical mechanisms overpredict NOx removal relative to long-lived methanol and carbon monoxide. All chemical mechanisms underpredict observed NOx by at least 30%, and further evaluation is necessary to refine simulation sensitivities to initial conditions and chemical rate uncertainties.

Citation: Henderson, B. H., Pinder, R. W., Crooks, J., Cohen, R. C., Hutzell, W. T., Sarwar, G., Goliff, W. S., Stockwell, W. R., Fahr, A., Mathur, R., Carlton, A. G., and Vizuete, W.: Evaluation of simulated photochemical partitioning of oxidized nitrogen in the upper troposphere, Atmos. Chem. Phys. Discuss., 10, 20125-20165, doi:10.5194/acpd-10-20125-2010, 2010.
 
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