Since the stratosphere is warmer than the troposphere the convection will halt when
the parcel of air reaches the tropopause, the top of the troposphere.
Not exact matches
However, many processes that remove water from the atmosphere (i.e. cloud formation and rainfall) have a clear functional dependence on the relative humidity rather than the total amount
of water (i.e. clouds form when
air parcels are saturated at their local temperature, not when humidity
reaches X g / m3).
Heat (not latent heat) is removed prior to condensation by conversion
of kinetic energy to potential energy which then provokes condensation and when the phase change occurs the release
of latent heat causes the
air parcel to rise a little further with additional conversion
of KE to PE until it
reaches the correct lapse rate temperature for its height and then it stops rising and begins to descend.