A fully convective monatomic ideal gas is an adiabatic stellar polytrope with index . Its polytropic mass-radius relation gives
At the base of a thin grey atmosphere, the stellar surface boundary condition and electron-scattering opacity give
The ideal-gas equation evaluated on the convective adiabat gives
Combining these relations,
The Stefan–Boltzmann law then gives
Deep in an optically thick grey atmosphere, write and retain the first spatial-gradient correction in the transfer equation:
Angular and frequency integration then gives the radiative diffusion flux
For a thin plane-parallel atmosphere, constant Rosseland mean opacity , negligible external irradiation, and radius nearly equal to , radiative equilibrium gives . Therefore
With hydrostatic balance , the equivalent pressure form is
where .
For , the angular moments are
and
Thus this angular form satisfies the Eddington closure approximation, , and
Part (i) gives . Substitution in yields
Matching powers of gives and , the latter being constant flux. Hence .
At the surface there is no incoming intensity. Applying this condition to the outgoing hemisphere in the moment approximation,
so . Consequently
Now and the effective temperature is defined by . It follows that
At the top of the grey atmosphere,
For a plane-parallel atmosphere in radiative equilibrium, constant surface gravity of a star and opacity , match the stellar structure interior where the radiative flux satisfies . The grey atmosphere law then puts the surface at optical depth with . Integrating hydrostatic equilibrium in optical depth from gives . Multiplication by proves the displayed boundary condition for , . At the integral is logarithmic and the continuous limit is . The relation assumes negligible radiation pressure and describes the Eddington closure approximation, rather than exact angular transfer.