“…When light-absorbing aerosols deposit on snow or ice surfaces, they may speed up the melting through the additional absorption of solar radiation (e.g., Flanner et al, 2007;Qian et al, 2011Qian et al, , 2015Warren & Wiscombe, 1980), which has additional important implications for climate change and seasonal distribution of water resource (e.g., Rahimi et al, 2019). The understanding of detailed physical and chemical processes for aerosols and their interactions with other components of the climate system has been obtained from laboratory experiments, field observations, or process modeling studies (e.g., Carslaw et al, 2013;Fanourgakis et al, 2019;Rosenfeld et al, 2014;Shilling et al, 2009;Shrivastava et al, 2015;Sorooshian et al, 2019;Wang et al, 2011). They are very challenging to treat accurately in Earth system models (ESMs) that are relied upon to represent and understand the complex global impact of aerosols and their interactions with the coupled aerosol-cloud-radiation-dynamics system (e.g., Mann et al, 2014;Gettelman, 2015;Zhang et al, 2016;Ghan et al, 2016;Gryspeerdt et al, 2017).…”