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Table 1

Parameters used in the different (retrieval) models, assumed true values, and prior distributions.

Parameter Description Truth Prior Model configuration
CF
aз P–T parameter (degree 3) 2.30(1) 𝒰(0, 10)
a2 PT parameter (degree 2) 29.83(1) 𝒰(0, 500)
a1 P–T parameter (degree 1) 125.64(1) 𝒰(0, 1000)
a0 P–T parameter (degree 0) 344.94(1) 𝒰(0, 1000)
log10(P0) Surface pressure [bar] 1.97(2) 𝒰(−4, 3) × ×
Rpl Planet radius [R] 0.95(2) 𝒢(0.95, 0.20)
log10(Mpl) Planet mass [M] −0.09(2) 𝒢(−0.09, 0.40)
log10(CO2) CO2 mass fraction −0.015(2) log10 (1 − 10𝒰(−7, 0)
log10(H2O) H2O mass fraction −4.699(2) 𝒰(−7, 0)
log10(CO) CO mass fraction −4.770(2) 𝒰(−7, 0)
H2SO4 cloud mass fraction −5.097(3) 𝒰(−7, −1) × ×
log10(H2Ocloud) H2O cloud mass fraction 𝒰(−7, −1) × × ×
Cloud top pressure [bar] −1.30(4) 𝒰(−6, 3) ×
Cloud thickness [bar] 0.161(4) 𝒰(−6, 3) ×
log10(Rcloud) Mean cloud particle radius [cm] −4.30(4) 𝒰(−8, −3) ×
σcloud Log-normal particle size spread 1.95(4) 𝒰(1, 5) ×

Notes. In the third column we provide the values used to generate the Venus-twin spectrum introduced in Sect. 2.1. These values provide the ground truth for all retrievals. The fourth column lists the prior distributions used in the retrievals. With 𝒰(x, y), we denote a boxcar prior with lower threshold x and upper threshold y; 𝒢(µ, σ) indicates a Gaussian prior with mean µ and standard deviation σ. The last four columns summarize the model parameters used by the different forward models in the retrievals ( = used, × = unused; see Sect. 2.3.2) and the model color-coding used throughout the paper. – opaque H2SO4 clouds (84% H2SO4, 16% H2O by weight); –transparent H2SO4 clouds (84% H2SO4, 16% H2O by weight); – opaque H2O clouds (100% H2O); ℳCF – cloud-free.

References. (1)Obtained by fitting Eq. (1) to the Venus P–T profile in Fig. 1 of Mueller-Wodarg et al. (2008); (2)Near surface abundances from NASA’s planet factsheet: https://nssdc.gsfc.nasa.gov/planetary/factsheet/venusfact.html; (3)Mean of values from Oschlisniok et al. (2012) and Krasnopolsky (2015); (4)Mean values for the mode 1 cloud particles in Titov et al. (2018).

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