Fig. 3

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Relative flux (Eq. (2)) at a wavelength, λ = 7μm, of the spherical approximation (batman) compared to the diffuse opacity of a 1D (Table 1) atmospheric simulation (Pytmosph3R) (see Fig. 2 for the schematics). The effect is similar in the case of a 2D day–night (Table 1) simulation (Pytmosph3R) without rotation (i.e., N𝒯 = 1). The same effect holds true in 3D cases, since the opacity of each case will decrease with the altitude, although it will be dominated by other effects.
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