Remote sensing of NO2
2.3.3 Radiative Transfer Equation: Diffuse part, plane surface

In calculating the diffuse part of the RTE we have to take into account the following components:

The loss as a result of extinction:

The gain as a result of multiple scattering:

The gain as a result of single scattering of solar radiation:

The gain as a result of reflection of light from the surface:

The gain as a result of emission:

where

θ zenith angle;
μ cos(θ);
φ azimuth angle;
ε emission coefficient (= absorption coefficient);
ζ scattering coefficient;
Fsol flux from the sun;
P weighted phase function for scattering;
A surface albedo;
B Planck radiation;
τ optical depth;
Top of page