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Fig. 4

image

Opacities for a chemical equilibrium atmosphere at 600 K (left) and 1400 K (right) at 0.1 bar. Toppanels: abundance-weighted opacities for a solar composition atmosphere.Bottom panels: abundance-weighted opacities for a 30x solar composition atmosphere. Carbon monoxide, water, methane, and carbon dioxide (for 30x solar) are the dominant absorbing species at the two IRAC channels (3.6 and 4.5 μm).

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