“…Aerosols influence cloud processes by serving as cloud condensation nuclei (CCN) on which cloud droplets can form (Köhler, 1936). The size of CCN determines the droplets' initial size distribution and hence impacts cloud processes and properties, such as size (Rosenfeld et al, 2008;Altaratz et al, 2014;Koren et al, 2014), lifetime (Albrecht, 1989), optical properties (Twomey and Squires, 1959;Twomey, 1977;Mülmenstädt and Feingold, 2018), and rain amounts and patterns (Yin et al, 2000b;Rosenfeld et al, 2006;Xue et al, 2008;Yuan, 2011;Altaratz et al, 2014;Koren et al, 2014;Seigel, 2014).…”