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

[摘要] 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.

[学科分类] 大气科学