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Examples
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Our simple script is logarithmic (remember our example of adding more shades over a window) but does not allow for complete saturation of radiative wavelengths, likely increases in evapo-transpirative cooling, increases in albedo (bright clouds reflecting more incoming solar radiation) nor any variation by latitude and so will progressively overestimate potential warming from CO2 alone.
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If weather gets more severe and the specific humidity increases with temperature, don’t convective and evapo-transpirative surface energy losses increase?
The "First" Assessed Likely Range for Climate Sensitivity « Climate Audit 2007
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