Fig. 11

Atmospheric temperature and entropy profiles when artificially shifting the temperature gradient (solid lines) and γ (dashed lines). The temperature and entropy profiles of 25 planets with masses from 3 M⊕ to 20 M⊕ (from bottom to top) with a fixed composition of 0.5% H–He mass fraction, 40% water mass fraction, and 59.5% of a rocky core. On the bottom, the profiles corresponding to a mass of 15 M⊕.
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