“…Once in the atmosphere, SA reacts with numerous precursor compounds at rates spanning several orders of magnitude to form stable particles. These compounds include ammonia (Coffman & Hegg, 1995; Hanson & Eisele, 2002), amines (Glasoe et al., 2015; Jen et al., 2014; Kurtén et al., 2008; Kürten et al., 2018), oxidized organics (Riccobono et al., 2012), alkanolamines (Fomete et al., 2022a), and ions (Eisele et al., 2006; Fomete et al., 2022b; Kirkby et al., 2011, 2016). In addition, methanesulfonic acid (MSA), which can exist in tandem with SA, has been shown to nucleate with and without SA in terrestrial and marine environments (Chen & Finlayson‐Pitts, 2017; Dawson et al., 2012; Elm, 2022; Johnson & Jen, 2023a; Saltzman et al., 1983).…”