@article { ISI:000335923300001,
	title = {An MCM modeling study of nitryl chloride (ClNO2) impacts on oxidation, ozone production and nitrogen oxide partitioning in polluted continental outflow},
	journal = {ATMOSPHERIC CHEMISTRY AND PHYSICS},
	volume = {14},
	number = {8},
	year = {2014},
	pages = {3789-3800},
	abstract = {Nitryl chloride (ClNO2) is produced at night by reactions of dinitrogen pentoxide (N2O5) on chloride containing surfaces. ClNO2 is photolyzed during the morning hours after sunrise to liberate highly reactive chlorine atoms (Cl center dot). This chemistry takes place primarily in polluted environments where the concentrations of N2O5 precursors (nitrogen oxide radicals and ozone) are high, though it likely occurs in remote regions at lower intensities. Recent field measurements have illustrated the potential importance of ClNO2 as a daytime Cl center dot source and a nighttime NOx reservoir. However, the fate of the Cl center dot and the overall impact of ClNO2 on regional photochemistry remain poorly constrained by measurements and models. To this end, we have incorporated ClNO2 production, photolysis, and subsequent Cl center dot reactions into an existing master chemical mechanism (MCM version 3.2) box model framework using observational constraints from the CalNex 2010 field study. Cl center dot reactions with a set of alkenes and alcohols, and the simplified multiphase chemistry of N2O5, ClNO2, HOCl, ClONO2, and Cl-2, none of which are currently part of the MCM, have been added to the mechanism. The presence of ClNO2 produces significant changes to oxidants, ozone, and nitrogen oxide partitioning, relative to model runs excluding ClNO2 formation. From a nighttime maximum of 1.5 ppbv ClNO2, the daytime maximum Cl center dot concentration reaches 1x10(5) atoms cm(-3) at 07:00 model time, reacting mostly with a large suite of volatile organic compounds (VOC) to produce 2.2 times more organic peroxy radicals in the morning than in the absence of ClNO2. In the presence of several ppbv of nitrogen oxide radicals (NOx = NO+NO2), these perturbations lead to similar enhancements in hydrogen oxide radicals (HOx = OH+HO2). Neglecting contributions from HONO, the total integrated daytime radical source is 17\% larger when including ClNO2, which leads to a similar enhancement in integrated ozone production of 15 \%. Detectable levels (tens of pptv) of chlorine containing organic compounds are predicted to form as a result of Cl center dot addition to alkenes, which may be useful in identifying times of active Cl center dot chemistry.},
	issn = {1680-7316},
	doi = {10.5194/acp-14-3789-2014},
	author = {Riedel, T. P. and Wolfe, G. M. and Danas, K. T. and Gilman, J. B. and Kuster, W. C. and Bon, D. M. and Vlasenko, A. and Li, S. -M. and Williams, E. J. and Lerner, B. M. and Veres, P. R. and Roberts, J. M. and JS Holloway and Lefer, B. and Brown, S. S. and Thornton, J. A.}
}
