If the Earth is treated as a spherical blackbody of radius 6371 km, absorbing heat from the Sun at a rate given by the solar constant (1370. W/m2) and immersed in space with an approximate temperature of Tsp = 50.0 K, it radiates heat back into space at an equilibrium temperature of 278.9 K. (This is a slight refinement of the model in Chapter 18.) Estimate the rate at which the Earth gains entropy in this model.
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