Exoplanet weather and climate regimes with clouds and thermal ionospheres - A model grid study in support of large-scale observational campaigns

Open Access

Fig. 5

Total nucleation rate, J_* = ∑_i J_i [cm⁻³ s⁻¹], i = TiO₂, SiO, NaCl, KCl, in the 2D equatorial plane (θ = 0°) for the 1D profiles extracted from the 3D GCM models for log₁₀g = 3 [cgs]. The same warm model atmospheres similar to Fig. 3 are depicted.

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