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Fig. B.3

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Outgoing thermal flux for a pure CO2 atmosphere on an Earth gravity planet (𝑔 = 9.81 m/s2) are shown for gray atmosphere model with different assumptions. The results of the full RT in a vertically extended atmosphere (“Full RT”) is used for benchmarking (solid lines). The models are compared for the same surface temperatures and pressures, where different surface pressures are indicated by variations in color. Left panel: Results of the gray atmosphere model is shown for ĸ0(CO2) = 0.001 m2/kg (dashed lines) and ĸ0(CO2) = 0.05 m2/kg (dash- dotted lines). Right panel: Results of the corrected gray atmosphere is shown (dash-dotted lines) in comparison to the Full RT calculations.

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