“…The WRF model configuration included the Morrison doublemoment scheme (Morrison et al, 2009), version 2 of the Kain-Fritsch cumulus scheme (Kain, 2004), the Asymmetric Convective Model version 2 (ACM2) planetary boundary layer (PBL) scheme (Pleim, 2007), the Pleim-Xiu land surface model (Xiu and Pleim, 2001), and the RRTMG shortwave and longwave radiation scheme (Iacono et al, 2008). The CMAQ model was configured using the Carbon Bond 2005 (CB05) chemical mechanism (Yarwood et al, 2005;Whitten et al, 2010) and the sixth-generation CMAQ aerosol module (AERO6) (Appel et al, 2013 (Gantt et al, 2014;He at al., 2015a, b;Glotfelty et al, 2017a, b;Glotfelty and Zhang, 2017) (Appel et al, 2013) using a horizontal resolution of 36 km covered most of China and parts of east Asia. The two-way coupled WRF-CMAQ used the same vertical resolution for WRF and CMAQ, i.e., 23σ layers from the surface to 100 hPa.…”