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Nighttime chemistry at a high altitude site above Hong Kong
Author(s) -
Brown Steven S.,
Dubé William P.,
Tham Yee Jun,
Zha Qiaozhi,
Xue Likun,
Poon Steven,
Wang Zhe,
Blake Donald R.,
Tsui Wilson,
Parrish David D.,
Wang Tao
Publication year - 2016
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1002/2015jd024566
Subject(s) - daytime , ozone , altitude (triangle) , environmental science , atmospheric sciences , aerosol , nitrogen , environmental chemistry , outflow , nox , mixing ratio , atmospheric chemistry , air quality index , seasonality , hydrology (agriculture) , chemistry , meteorology , geography , combustion , geology , statistics , geometry , mathematics , organic chemistry , geotechnical engineering
Abstract Nighttime reactions of nitrogen oxides influence ozone, volatile organic compounds, and aerosol and are thus important to the understanding of regional air quality. Despite large emissions and rapid recent growth of nitrogen oxide concentrations, there are few studies of nighttime chemistry in China. Here we present measurements of nighttime nitrogen oxides, NO 3 and N 2 O 5 , from a coastal mountaintop site in Hong Kong adjacent to the megacities of the Pearl River Delta region. This is the first study of nighttime chemistry from a site within the residual layer in China. Key findings include the following. First, highly concentrated urban NO x outflow from the Pearl River Delta region was sampled infrequently at night, with N 2 O 5 mixing ratios up to 8 ppbv (1 min average) or 12 ppbv (1 s average) in nighttime aged air masses. Second, the average N 2 O 5 uptake coefficient was determined from a best fit to the available steady state lifetime data as γ (N 2 O 5 ) = 0.014 ± 0.007. Although this determination is uncertain due to the difficulty of separating N 2 O 5 losses from those of NO 3 , this value is in the range of previous residual layer determinations of N 2 O 5 uptake coefficients in polluted air in North America. Third, there was a significant contribution of biogenic hydrocarbons to NO 3 loss inferred from canister samples taken during daytime. Finally, daytime N 2 O 5 mixing ratios were in accord with their predicted photochemical steady state. Heterogeneous uptake of N 2 O 5 in fog is determined to be an important production mechanism for soluble nitrate, even during daytime.