Fig. 5
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TRAPPIST-1 g: Net flux (OLR-ASR) evolution for the magma ocean scenarios shown in Fig. 4; that is, for 1 TO, 5 TO, and 100 TO initial H2O and various initial CO2 mass fractions for an albedo of 0. We note simulations with an assumed albedo of 0.75 (not shown) are qualitatively similar but have a shorter regime with net flux limited by the runaway greenhouse radiation limit.
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