Along a ray, the radiative transfer equation has the formal solution of the radiative transfer equationfor each isothermal region in local thermodynamic equilibrium, neglecting scattering. For a self-luminous atmosphere with no incident intensity from below at the relevant photosphere, and in the optically thick limit, .
The observed radiative flux is the projected-disc integralThe inner region occupies projected fraction , henceFor finite optical depths, each Planck law function in this formula is replaced by its corresponding emergent intensity above.
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