the aerosol-aware Thompson–Eidhammer microphysics scheme has been implemented in
the WRF-Chem to quantify and evaluate the effect of dust on the ice nucleation process in
the atmosphere by serving as ice nuclei (IN). The performance of the GOCART–Thompson
microphysics scheme in simulating the effect of dust in atmospheric ice nucleation is then
evaluated over East Asia during spring, a typical dust-intensive season, in 2012. Based …