Secondary organic aerosols (SOA) have been an active area of research over the past decades with the goal of improving their representation in air quality and climate models (Hodzic et al., 2016; Tsigaridis et al., 2014), which is essential for predicting their effect on human health (Mauderly & Chow, 2008) and their contribution to radiative forcing in the climate system (Boucher et al., 2013). The misrepresentation of SOA formation pathways in 3D models has led to a long-standing discrepancy between observed and modeled organic aerosol concentrations that has been reported from urban to remote regions (de Gouw, 2005;Hodzic et al., 2020). Unlike sulfate and other inorganic aerosols, which are made from a few dominant chemical pathways, SOAs result from the condensation of a very large number of partly oxidized gases. These gases are generated from the multi-generational oxidation of volatile organic compounds (VOCs) emitted from anthropogenic and natural sources. This complexity is not included in current 3D models that rely on simplified SOA parameterizations that have been developed and