where L is the optical path length between the points at which 
E and 
E0 are measured and 
k0 is the wave number in free space. In weakly absorbing media, 
N = n, K = κ, and 
α = 0. If the 
Use corrections for strongly absorbing media check box is selected, 
N is the real part of the apparent refractive index, 
K is the complex part of the apparent refractive index, and 
α is the angle between the surfaces of constant amplitude and surfaces of constant phase; both of these concepts are explained in 
Refraction in Strongly Absorbing Media. The ray intensity and power are both proportional to the square of the electric field norm, so these quantities change according to the relations
 
    where c is the speed of light in the medium and 
si,0 is value of one of the Stokes parameters of the ray before the effects of changes in the principal radii of curvature have been applied.
 
    
    Despite requiring an extra degree of freedom per ray, the advantage of Equation 3-21 over 
Equation 3-20 is that the dependent variables in 
Equation 3-21 all vary linearly within a homogeneous medium. This makes 
Equation 3-21 less prone to numerical stiffness; it remains more accurate when the solver takes long time steps, compared to 
Equation 3-20, potentially reducing solution time and improving accuracy.