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Fig. 12

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Simulated spectra for the TRAPPIST-1 planet: Emitted (top: MIR, R = 400), reflected (middle: NIR, R = 400), and transmitted light (bottom: NIR-MIR, R = 200). Note. MIR features in emission are not just dependent on the abundance of spectrally active gases, but also the temperature structure of the atmosphere. Left panel: anoxic, abiotic scenario (Tsurf = 275 K): CO flux of 109 (black), 1010 (magenta), and 1012 molecules cm−2 s−1 (blue), corresponding to lightning flash rates of ~2, ~35 and ~1500 times modern Earth’s, respectively. Right panel: oxic, biotic scenario (Tsurf = 288 K): CO flux of 108 (black) and 1011 molecules cm−2 s−1 (blue), corresponding to lightning flash rates of ~0.9 and ~680 times modern Earth’s, respectively.

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