Vertical profiles of diabatic heating rates for the run cases with T_eff = [400, 500, 600] K and P_rot = 20 h at t_run = 1000 d. Overlaid are convective zones and cloud condensate layers, intended to give an overview of the physical processes that contribute to the radiative balance of the atmospheres under study. The smaller panels on the right-hand side shows the extent of each overplotted layer.