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Christina M. Patricola, R. Saravanan, and Ping Chang

used: the Kain–Fritsch cumulus, Lin et al. microphysics, the Rapid Radiative Transfer Model for general circulation models (RRTMG) longwave radiation, Goddard shortwave radiation, Yonsei University (YSU) planetary boundary layer using a Monin–Obukhov surface scheme, and the Noah land surface model. WRF is configured with a horizontal resolution of 27 km and 28 levels in the vertical reaching to 50 hPa on a domain ( Fig. 1 ) covering the Atlantic sector. The model time step is 90 s, and output is

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