1943 Volume 21 Issue 5 Pages 251-259
Consider a vertical air column of depth h. The pressure is p0 at the ground and pn, at the top. The lower part from p0 to pi (pn<pi<p0) is saturated and ascends wet-adiabatically, while the upper part from pi to pn descends dry-adiabatically. A constant lapse-rate α is assumed, and at the boundary pi there exists no discontinuity of temperature, therefore the energy releasable by such an overturning, if any, is nothing but the moist-labile (feuchtlabile) energy.
The energy equation has been derived and the result of numerical evaluation is as follows:
It is seen here that the moist-labile energy is generally very small in the atmosphere of conditional instability.