This is what I would say delineates
the various atmospheric layers.
Not exact matches
θ = potential temperature, which is conserved for dry adiabatic processes and is a useful vertical coordinate for examining
various fluid mechanical processes (like Rossby waves) when the
atmospheric lapse rate is stable (for dry convection)(which is generally true on a large scale away from the boundary
layer).
The short - term influence of
various concentrations of
atmospheric carbon dioxide on the temperature profile in the boundary
layer.
After looking at the
various elements of the climate models, they judged that there was little to do with the dynamical core of the
atmospheric model (that it was quite mature and performing quite well), although there were issues with the parameterizations of convection and the
atmospheric boundary
layer.