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Radiative Transfer Radiative transfer equation (RTE) - IAP ...

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<strong>Radiative</strong> <strong>transfer</strong> <strong>equation</strong><br />

Schwarzschild <strong>equation</strong><br />

Interpretation:<br />

I (0) = I (τ)e −τ +<br />

∫ τ<br />

0<br />

Be −τ ′ dτ ′<br />

◮ I (τ) emission at level τ, e.g. by surface of the Earth, or<br />

any other level where opacity is τ when looking down<br />

from sensor<br />

◮ but reduced by the absorption along the path to the<br />

sensor by e −τ , i.e. the transmissivity<br />

◮ plus emission of atmospheric layers Bdτ ′<br />

◮ Note: Planck function depends on T , B = B(T (τ))<br />

◮ taking into account attenuation on the way to the<br />

sensor e −τ ′<br />

☞ Almost all radiative <strong>transfer</strong> problems involving<br />

emission and absorption, without scattering, can be solved<br />

with this <strong>equation</strong><br />

<strong>RTE</strong><br />

Beer’s law<br />

Abs. cross section<br />

Opacity &<br />

Transmission<br />

Mean free path<br />

Scattering<br />

Schwarzschild eq.

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