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Derek J. Posselt and Tomislava Vukicevic

saturation with respect to liquid at temperatures above freezing and with respect to ice below. Time-evolving profiles of vertical motion and water vapor forcing ( Figs. 1b,c , respectively) consistent with observed and simulated squall-line-type evolution ( Moncreiff 1992 ; Fovell and Tan 1998 ; Houze 2004 ) are used to drive the simulation. The model is run with 60 vertical layers with constant 250-m vertical grid spacing and a 5-s time step, and the radiative transfer, surface flux, and

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