Including CO2 ice albedo in a 1D energy balance model raises the starlight required for F-dwarf planets to exit a snowball state by about 29 percent relative to water-ice-only models.
Mudball: Surface dust and Snowball Earth deglaciation
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A One-Dimensional Energy Balance Model Parameterization for the Formation of CO2 Ice on the Surfaces of Eccentric Extrasolar Planets
Including CO2 ice albedo in a 1D energy balance model raises the starlight required for F-dwarf planets to exit a snowball state by about 29 percent relative to water-ice-only models.