Not exact matches
Another important paper of recent is by Easterling and Wehner that
demonstrates that
cooling on timescales of years to a decade or two are not that unusual even when the system is undergoing a long - term warming trend induced by
radiative forcing.
It's true that there are aspects of the vertical distribution of
radiative cooling that can't be controlled by adjusting the air - sea temperature difference, but I haven't seen it
demonstrated that these are crucial.
Of course, Wallace & Hobbs (Atmospheric Science, Second Edition: An Introductory Survey) cited Manabe & Strickler and
demonstrated that convection tends to warm the upper troposphere and
cool the lower troposphere beyond
radiative only atmosphere: