There can / will be local and regional, latitudinal, diurnal and seasonal, and internal variability - related deviations to the
pattern (in temperature and in optical properties (LW and SW) from components (water vapor, clouds, snow, etc.) that vary with weather and climate), but the global average effect is at least somewhat constrained by the global average
vertical distribution of solar heating, which requires the equilibrium net convective + LW fluxes, in the global average, to be sizable and upward at all levels from the surface to TOA, thus tending to limit the extent and magnitude of inversions.)
«The global mean climate responses to different forcings may differ because of the character of the forcings themselves (such as their geographical or
vertical distribution) and because different forcings induce different
patterns of surface warming or cooling, thereby affecting the net top - of - atmosphere radiation imbalance, and thus the ocean heat uptake rate.»