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The vertical P-velocity in a state of saturation is derived from the equation of vertical P -vorticity and the conservation of the equivalent potential temperature . The difference of vertical P-velocities in the dry and wet adiabatic processes are estimated. In the last section of this paper, the comment of the effects of condensation on the hight change are explained.

On the Calculation of the Vertical pvelocitq Concerning the Wet Adiabatic Process