Nitrate, formed in the atmosphere via gas-to-particle conversion of NO x and HNO 3 , plays an important role in the Earth's climate (Boucher et al., 2013;Szopa et al., 2021). It can affect the Earth's radiation budget directly through scattering solar radiation (e.g., Adams et al., 2001;van Dorland et al., 1997) and indirectly through acting as cloud condensation nuclei (CCN; e.g., Kulmala et al., 1993;Xu & Penner, 2012). The formation of nitrate aerosols can also impact atmospheric chemistry. Ammonium nitrate forms predominantly in the fine aerosol mode through the aqueous phase reaction between HNO 3 and excess NH 3 (left after fully neutralizing sulfate) (e.g., Bassett & Seinfeld, 1983;Metzger et al., 2002). Nitrate aerosols can also form in the coarse aerosol mode through heterogeneous reactions of nitrogen species such as HNO 3 and N 2 O 5 on the surface of mineral dust and