Let increase downward and let be the outward direction cosine. Assume a plane-parallel, static, nonscattering atmosphere in local thermodynamic equilibrium, so the source function is . Hydrostatic balance gives
The formal solution of the radiative transfer equation between , corresponding to , is
For an isothermal atmosphere, is constant and
If the lower boundary is itself thermalized, and the upward intensity remains the blackbody value.

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