“…Similarly, the vast majority of studies to date on NPF and C SOA from the dark ozonolysis of monoterpenes have been conducted at fixed and uncharacteristically low levels of RH that are not representative of the lower troposphere [19], which is where most of the NPF and C SOA are hypothesized to occur [9,[20][21][22][23][24][25]. Recently, studies have been reported to better understand the role of RH in NPF and SOA generation from the ozonolysis of several monoterpenes, including αand β-pinene [26][27][28][29][30][31], limonene [27,28], and 3 ∆-carene [27,28]. Reported results have been contradictory, with some reporting an enhancement in NPF and C SOA as a result of higher RH [27,[31][32][33], while others report Air 2023, 1 223 sharp decreases [28,31,[34][35][36][37][38].…”