Yang, H. and Pierrehumbert, R. T. 1994: Production of dry air by
isentropic mixing.
Not exact matches
Pierrehumbert, R. T. and Yang, H. 1993: Global chaotic
mixing on
isentropic surfaces.
If instead the vertical integral of the potential temperature is kept fixed — as argued by several authors to be appropriate in the case of convective
mixing — an
isentropic profile results.
With
mixing comes an overall tendency toward an intermediate profile between
isentropic and isothermal — no GHG's involved...
Radiative equilibrium does drive towards an isothermal state, but
mixing goes towards an
isentropic state, which is a recognized term indicating constant potential temperature (also dry adiabatic) because the log of potential temperature is basically the entropy in thermodynamic terms.
If you take an isothermal gas in gravity and thoroughly
mix it, it turns
isentropic.