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E. P. Nowottnick, P. R. Colarco, S. A. Braun, D. O. Barahona, A. da Silva, D. L. Hlavka, M. J. McGill, and J. R. Spackman

) in the SACM simulation ( Fig. 11c ) than in the SA simulation ( Fig. 11b ). Modifications to ice cloud effective radius are known to impact the radiative budget of the atmosphere ( Quaas et al. 2008 ; Rotstayn 1999 ; Jones and Slingo 1996 ), and in Fig. 12 the shortwave aerosol, longwave cloud, and net (shortwave plus longwave) total atmospheric radiative forcings are shown for the SA and SACM simulation at 1300 UTC 13 September 2012. The shortwave forcing is nearly identical in both

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