During recent years, aggressive air pollution mitigation measures in northern China have resulted in considerable changes in gas and aerosol chemical composition. But it is unclear whether aerosol water content and acidity respond to these changes. The two parameters have been shown to affect heterogenous production of winter haze aerosols. Here, we performed thermodynamic equilibrium modeling using chemical and meteorological data observed in urban Beijing for four recent winter seasons and quantified the changes in the mass growth factor and pH of inorganic aerosols. We focused on high relative humidity (> 60%) conditions when submicron particles have been shown to be in the liquid state. From 2014/2015 to 2018/2019, the modeled mass growth factor decreased by about 9%-17% due to changes in aerosol compositions (more nitrate and less sulfate and 18 Hence, it is useful to characterize these two parameters for understanding haze formation. 48 A general approach to measuring aerosol water content is by perturbing RH and detecting the 49 changes in aerosol physical properties, e.g., using nephelometers or hygroscopicity tandem 50 differential mobility analyzers, 3,19,20 but such measurements are not performed routinely in China. Another common approach involves thermodynamic equilibrium analyses between gas and aerosol phase for semivolatile species, requiring composition measurements and a thermodynamic model (e.g., E-AIM or ISORROPIA). 2,21,22 Intercomparisons indicate that water contents estimated