The Lambertian in a Given Direction apodization type scales all source rays by their direction to give a Lambertian intensity distribution. This effectively apodizes the rays with a cos(f) factor, where f is the elevation angle in polar coordinates. The following images show the source and intensity distribution for an isotropic plane of random rays emitting into a 90o cone half angle with the Lambertian in a Given Direction apodization applied.
The Lambertian in a Given Direction directional apodization is available on the Power tab of a Detailed Source dialog. From the Power tab, select "Lambertian in a Given Direction" from the drop down menu of directional apodization types.
The following table describes the available controls on the Power tab of a Detailed Source dialog. Of interest to this help topic are the Direction Apodization parameter settings.
Generating a Lambertian distribution Using the Lambertian in a Given Direction apodization is radiometrically equivalent to selecting a Uniform Direction apodization and setting the source rays to be Lambertian on the Positions / Directions tab of the source dialog. Although these two methods of generating a Lambertian source are radiometrically equivalent, they are represented by different distributions of rays. The Lambertian option on the Positions / Directions page distributes the rays equally in direction cosine space and the Isotropic option on the Positions / Directions page distributes the rays equally in angle space.
Direction Apodization - Uniform Unit Apodization Direction Apodization - Inverse Lambertian in a given direction Direction Apodization - Gaussian Direction Apodization - cos^n or sin^n in a given direction Direction Apodization - Sampled as a function of Spherical Angles
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