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Philip T. Bergmaier and Bart Geerts

model ( Chen and Dudhia 2001 ). The Kain–Fritsch cumulus scheme ( Kain and Fritsch 1990 , 1993 ; Kain 2004 ) was used for the 12-km domain only, allowing convection to be explicitly resolved in the innermost two domains. For model microphysics, the Predicted Particle Property (P3) microphysics scheme ( Morrison and Milbrandt 2015 ) has been implemented, which is coupled with the Rapid Radiative Transfer Model for GCMs (RRTMG) longwave and shortwave radiation schemes ( Iacono et al. 2008 ). Several

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