

Data comes from NASA planetary fact sheets (amazing resource btw).
Overall equation structure:
Circular area that can receive sunlight: pi x radius ^ 2
Total incoming power : solar irradiance x circular area
Spherical area : 4 x pi x radius ^ 2
Black body radiation : stefan-boltzmann constant x Area x Temperature ^ 4
You know have incoming power and outgoing power.
Percentage : 100 x (Outgoing - incoming) / outgoing
The greenhouse effect still has a limit to how much it can trap.
At the end of the day infrared radiation is still basically light.
Even on the cloudiest day, or when there is super dense smoke or ash, it is still not pitch black out. Some light gets through. If you are looking into a mirror, it might seem like it reflects 100% of light. But they only reflect around 95%.
You would require something which can let through 100% of all sunlight, but still trap 99.5% from leaving.
You could have a look at how one-way mirrors work, to understand the percentages of light passed through and reflected.