Transition from high- to low-NOx control of night-time oxidation in the southeastern US

• Published in: Nature geoscience Vol. 10; no. 7; pp. 490 - 495
• Main Authors: Edwards, P. M., Aikin, K. C., Dube, W. P., Fry, J. L., Gilman, J. B., de Gouw, J. A., Graus, M. G., Hanisco, T. F., Holloway, J., Hübler, G., Kaiser, J., Keutsch, F. N., Lerner, B. M., Neuman, J. A., Parrish, D. D., Peischl, J., Pollack, I. B., Ravishankara, A. R., Roberts, J. M., Ryerson, T. B., Trainer, M., Veres, P. R., Wolfe, G. M., Warneke, C., Brown, S. S.
• Format: Journal Article
• Language: English
• Published: London Nature Publishing Group UK 01-07-2017; Nature Publishing Group
• Subjects: 704/172/169/824; 704/172/4081; Anthropogenic factors; Atmospheric chemistry; Chemical speciation; Cycles; Daytime; Earth Sciences; Earth System Sciences; Geochemistry; Geology; Geophysics/Geodesy; Human influences; Lower atmosphere; Night; Nitrogen compounds; Nitrogen oxides; Nitrogen oxides emissions; Organic compounds; Oxidation; Oxides; Ozone; Photochemicals; Pollutants; Ratios; VOCs; Volatile organic compounds; United States > US
• ISSN: 1752-0894; 1752-0908
• DOI: 10.1038/ngeo2976

The influence of nitrogen oxides (NO
x
) on daytime atmospheric oxidation cycles is well known, with clearly defined high- and low-NO
x
regimes. During the day, oxidation reactions—which contribute to the formation of secondary pollutants such as ozone—are proportional to NO
x
at low levels, and inversely proportional to NO
x
at high levels. Night-time oxidation of volatile organic compounds also influences secondary pollutants but lacks a similar clear definition of high- and low-NO
x
regimes, even though such regimes exist. Decreases in anthropogenic NO
x
emissions in the US and Europe coincided with increases in Asia over the last 10 to 20 years, and have altered both daytime and nocturnal oxidation cycles. Here we present measurements of chemical species in the lower atmosphere from day- and night-time research flights over the southeast US in 1999 and 2013, supplemented by atmospheric chemistry simulations. We find that night-time oxidation of biogenic volatile organic compounds (BVOC) is NO
x
-limited when the ratio of NO
x
to BVOC is below approximately 0.5, and becomes independent of NO
x
at higher ratios. The night-time ratio of NO
x
to BVOC in 2013 averaged 0.6 aloft. We suggest that night-time oxidation in the southeast US is in transition between NO
x
-dominated and ozone-dominated.
The influence of NO
x
levels at night on atmospheric oxidation is unclear. Analyses of aircraft observations suggest that night-time oxidation is transitioning from a high- to low-NO
x
regime in the southeast US due to declines in NO
x
levels.