Math 2.0

Astronomy and astrophysics Example

Radiative transfer equation

Example

Let D⊆ℝ3D \subseteq \R^3 be a region filled with a medium, and let S2S^2 be the unit sphere of directions. The unknown is the specific intensity I(x,Ω)I(x, \Omega) of radiation at a point x∈Dx \in D travelling in the direction Ω∈S2\Omega \in S^2, at one fixed frequency. Let κ(x)≥0\kappa(x) \ge 0 and σ(x)≥0\sigma(x) \ge 0 be the absorption and scattering coefficients, B(x)B(x) the emission source, and p(Ω′⋅Ω)≥0p(\Omega' \cdot \Omega) \ge 0 the phase function, normalized by 14π∫S2p(Ω′⋅Ω) dΩ′=1\frac{1}{4\pi} \int_{S^2} p(\Omega' \cdot \Omega) \, d\Omega' = 1. The stationary radiative transfer equation is Ω⋅∇xI(x,Ω)+(κ(x)+σ(x))I(x,Ω)=κ(x)B(x)+σ(x)4π∫S2p(Ω′⋅Ω) I(x,Ω′) dΩ′.\Omega \cdot \nabla_x I(x, \Omega) + \big(\kappa(x) + \sigma(x)\big) I(x, \Omega) = \kappa(x) B(x) + \frac{\sigma(x)}{4\pi} \int_{S^2} p(\Omega' \cdot \Omega) \, I(x, \Omega') \, d\Omega'. It contains a derivative of II along the direction Ω\Omega and an integral of II over all directions. So it is an integro-partial differential equation.

Check: if κ\kappa, σ\sigma and BB are constant, the constant intensity I=BI = B is a solution. The left side is (κ+σ)B(\kappa + \sigma) B, and by the normalization of pp the right side is κB+σB\kappa B + \sigma B.

Remarks

The left side describes the loss of intensity along a ray by absorption and by scattering out of the direction Ω\Omega. The right side describes thermal emission and scattering into Ω\Omega from all other directions. Along each ray x+sΩx + s\Omega the equation is a linear ordinary differential equation, and integrating it turns the problem into an integral equation for II. For a plane-parallel atmosphere with isotropic scattering this leads to equations such as the Milne problem.

Where this leads

2 pages build on this one.

Further reading

  1. Web https://en.wikipedia.org/wiki/Radiative_transfer
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