This suggests that the well - known changes in temperature lapse rates associated with the tropopause / stratosphere regions are related to the phase change, and not «ozone heating», which had been the previous explanation. (oprj.net)
In the GCM, if a layer is statically unstable relative to a specified convective temperature lapse rate, a convection scheme relaxes temperatures in that layer toward an enthalpy - conserving profile with the convective lapse rate. (climate-dynamics.org)
This is somewhat compensated by the negative temperature lapse rate feedback that weakens the greenhouse effect. (climate-dynamics.org)