“…Many factors dictate the extent to which Cl − depletion occurs in an air mass, including meteorology (e.g., wind speed; temperature; relative humidity, RH; and available solar radiation), the size distribution and mixing state of sea salt particles, and the availability and length of exposure to surrounding acidic species (Su et al, 2022, and references therein). Regarding the latter, Cl − depletion is therefore typically observed where marine particles and acidic species are both present, such as where emissions from biomass burning (BB) advect over a marine location (Braun et al, 2017;Maudlin et al, 2015;Li et al, 2003;Yokelson et al, 2009;Akagi et al, 2013;Dang et al, 2022;Crosbie et al, 2022); in regions with active phytoplankton and marine bacteria that emit dimethyl sulfide (DMS), which can oxidize to form sulfuric acid (H 2 SO 4 ; Seinfeld and Pandis, 2016;Tang et al, 2019;Yan et al, 2020); and/or in and around urban coastal environments (e.g., Kong et al, 2014;Chatterjee et al, 2020;AzadiAghdam et al, 2019;Nolte et al, 2008) where anthropogenic emissions serve as precursors for various acidic species.…”