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Presenterjacob.shpund (Unlicensed)

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Overall, the P3 microphysics shows a comparable climatology to MG2. P3 improves both the cloud shortwave and longwave radiative forcing in the Northern Hemisphere and the high cloud fraction in the Tropics. The ice water path is increased with P3 compared with MG2, and the frequency of heavy precipitation rates over the continental US is larger with P3 and more consistent with observations.  There are specific areas needed further improvements such as relatively low liquid water content at midlatitudes, and low-cloud fractions over the Southern Hemisphere.04

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