Geometric albedo model results including condensation, produced by sampling over the input parameter prior distributions (see Table 5) and using a scaling factor distribution to move the model away from chemical equilibrium. The wavelength-dependent albedos were then bandpass-integrated to produce the expected albedos in the TESS (orange) and CKC (blue) band. We find that high albedos are reachable with high metallicites, due to condensation removing the effect of metals from the upper atmosphere.