Vertical profile of temperature [Manabe & Strickler 1964 JAS]

Stratosphere: radiative equilibrium
Absorption of solar rad. (ozone) - emission of terr. rad. (CO2) = 0
Troposphere: radiative-convective equilibrium
Absorption - emission + convective heating (incl. condensation) = 0
Lapse rate is determined by convection (assumed to be constant).