“…Theoretical (Peeters et al, 2009;da Silva et al, 2010;Peeters and Müller, 2010;Peeters et al, 2014;Wang et al, 2018;Møller et al, 2019) and experimental studies (Crounse et al, 2011;Berndt, 2012;Crounse et al, 2012;Wolfe et al, 2012;Fuchs et al, 2013;Fuchs et al, 2014;Teng et al, 2017;Berndt et al, 2019;Novelli et al, 2020) have 25 hypothesized and found significant regeneration of OH radicals from unimolecular reactions of organic peroxy radicals (RO 2 , R = organic group) originating from the oxidation of biogenic VOCs such as isoprene, methacrolein, and methyl vinyl ketone (MVK). Although the inclusion of these new reaction paths in atmospheric chemical models can increase the predicted concentration of OH considerably, for example by a factor of three over tropical forests (Novelli et al, 2020), it is often not enough to explain the high OH concentrations observed in field experiments in areas characterized by high 30 isoprene emissions (Stone et al, 2011;Lu et al, 2012;Stone et al, 2012;Fuchs et al, 2013;Lu et al, 2013;Feiner et al, 2016;Lew et al, 2020).…”