Notes. For all parameters, we adopted uniform or log-uniform priors (shown as 𝒰) where the lower and upper boundaries are represented. ^(a)P_phot is the pressure for τ = 1 and ^(b)T_connect is the uppermost temperature of the photospheric layer, calculated by setting τ = 0.1 in the Eddington approximation (see Mollière et al. 2020). The priors for T₃, T₂, and T₁ were set to ensure a temperature profile that decreased monotonically with altitude to avoid temperature inversions. ^(c)$\log \left({\tilde{\text{X}}}_{\text{C}}\right)$ represents the scaling factor for the cloud mass fraction for each of the cloud species used in our retrieval (i.e., Al₂O₃, Fe, and MgSiO₃), defined such that $\log \left({\tilde{\text{X}}}_{\text{C}}\right)=0$ refers to a fraction equal to the equilibrium mass fraction.