| (1) |
For an atmosphere in LTE, we can assume that the source function is equal to the Planck
radiation function, so Sl(z) = Bl(z).
Unfortunately, it is not sufficient to know Sl as a function of physical depth
z; we must convert the physical depth scale to an optical depth scale:
| (2) |
| 1 | Calculate Sl(z) | 4 | Calculate optical depth scale |
| 2 | Calculate continuous opacity | 5 | Effect of large scale mass motion |
| 3 | Calculate line opacities. | 6 | Numerical integration of radiative |
| This requires: | transfer equation (1) | ||
| * line strengths | 7 | Non-plane parallel corrections | |
| * damping | |||
| * thermal and mass motion |