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The influence of nitrogen oxides (NOx) on daytime atmospheric oxidation cycles is well known, with clearly defined high- and low-NOxregimes. During the day, oxidation reactions—which contribute to the formation of secondary pollutants such as ozone—are proportional to NOxat low levels, and inversely proportional to NOxat high levels. Night-time oxidation of volatile organic compounds also influences secondary pollutants but lacks a similar clear definition of high- and low-NOxregimes, even though such regimes exist. Decreases in anthropogenic NOxemissions 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 NOx-limited when the ratio of NOxto BVOC is below approximately 0.5, and becomes independent of NOxat higher ratios. The night-time ratio of NOxto BVOC in 2013 averaged 0.6 aloft. We suggest that night-time oxidation in the southeast US is in transition between NOx-dominated and ozone-dominated.