Non-methane volatile organic compounds (VOCs) are ubiquitous and highly reactive in the atmosphere, contributing to the formation and removal of secondary organic aerosol (SOA) and greenhouse gases (Faiola et al., 2018;Kesselmeier & Staudt, 1999). Biogenic sources of VOCs dominate the global budget, contributing to 1,150 TgC yr −1 relative to the 142 TgC yr −1 from anthropogenic sources (Guenther et al., 1995;Singh, 1995). Of those biogenic sources, monoterpene isomers (C 10 H 16 ) constitute 15% of the emissions (Guenther et al., 2012). Despite structural similarities, different monoterpene isomers have different atmospheric reactivities (e.g., Atkinson, 1990), and our understanding of these isomers are further complicated by the differences in the factors that influence their emissions. Monoterpene emissions are influenced by several abiotic factors, the most well-known including temperature (e.g.,