Not exact matches
But if the optical thickness in that band is sufficiently smaller than in another band (depending on wavelengths), adding some absorption to the optically - thinner band would tend to result in warming of the colder layers (as there would be less
temperature variation over height in radiative equilbrium for that band,
given the same
surface (+ tropospheric)
temperatures.
Given BP, SL, and sea
surface temperature fields, good estimates of full - column HC
variations can be made at low and middle latitudes.
How the Earth's
surface temperature adjusts to a
given change in solar radiation depends on the processes by which the climate system responds to
variations in the energy it receives.
It is a
given that the existing models do not fully incorporate data or mechanisms involving cloudiness or global albedo (reflectivity)
variations or
variations in the speed of the hydrological cycle and that the variability in the
temperatures of the ocean
surfaces and the overall ocean energy content are barely understood and wholly inadequately quantified in the infant attempts at coupled ocean / atmosphere models.