Thursday, 16 January 2020: 4:45 PM
207 (Boston Convention and Exhibition Center)
Field observations over the last decade have demonstrated that nitryl chloride, ClNO2, is a major product of the nighttime heterogeneous uptake of N2O5in the lower atmosphere. Morning photolysis of ClNO2following its overnight production represents a large source of reactive chlorine. This mechanism is important in regionally polluted environments with elevated levels of nitrogen oxides (NOx= NO + NO2) that react to produce N2O5at night, and it is prevalent during the winter season when N2O5represents the dominant pathway for NOxoxidation. Recent aircraft campaigns have investigated ClNO2and N2O5in the urban winter atmosphere. The WINTER (Wintertime Investigation of Transport Emissions and Reactivity) campaign surveyed urban regions and outflow over the Eastern U.S. during the winter of 2015 using the NSF C130 aircraft. The UWFPS (Utah Winter Fine Particulate Study) campaign was an intensive study of regional air pollution in the urban mountain basins of Northern Utah, including Salt Lake City, using the NOAA Twin Otter aircraft. Both campaigns included measurements of nitrogen oxides, ozone, N2O5, ClNO2and aerosol composition that allow for detailed analysis of the factors governing N2O5uptake and ClNO2production. Yields of ClNO2from both campaigns show that it differs considerably from current parameterizations used in models, suggesting more complexity in ClNO2formation chemistry than has been represented from laboratory studies to date. This presentation will survey results from these campaigns, implications for the role of halogens in urban winter environments, and needs for further research to define wintertime heterogeneous chemistry of nitrogen oxides and halogens.
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