Fig. 10

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Radiative cooling and heating rates against radial distance for the CHAIN runs of the H2O atmospheres of planets b (top panel), c (middle panel), and d (bottom panel). The rates are shown between 1 and 4 Rpl, where most of the photochemistry takes place; higher altitudes are dominated by adiabatic expansion. For individual cooling processes, we only show those that contribute at least 5% to the total cooling rates (at some specific altitude). The line styles are explained in the legends, where the notation is the following: Ctot – total cooling rate (the sum of all radiative processes); Htot – total heating rate; μbar – the altitude corresponding to 1 μbar pressure level; X line – line cooling of the X element; molecule – the sum of molecule cooling processes (dominated by H2O molecule cooling); free-free H – bremsstrahlung cooling from hydrogen and helium.
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