Past exam of the physics course of the year 4 of the natural sciences course of the University of Cambridge / 2014 / Paper 1 / A1 / Solution

The solar flux at Earth is $\sigma T_{\odot }^4{R}_{\odot }^2/L^2$. A spherical Earth intercepts sunlight over its cross section but radiates over its whole surface, givingThis is below the observed mean surface temperature. Atmospheric infrared absorption and emission produce a greenhouse effect that raises the surface temperature relative to the effective radiating temperature. Including reflected sunlight alone would lower the estimate further; albedo does not explain a warmer surface.^[ref]