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Atmospheric light scattering: Difference between revisions
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→Light scattering during the day
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The altitude-dependent light reduction due to the clouds is the first instance of the <b>lightfield</b> technique, i.e. that the sunlight is represented as a series of functions r(x,y,z), g(x,y,z), b(x,y,z) in which the individual color channels are functions of vertex position in the scene. | The altitude-dependent light reduction due to the clouds is the first instance of the <b>lightfield</b> technique, i.e. that the sunlight is represented as a series of functions r(x,y,z), g(x,y,z), b(x,y,z) in which the individual color channels are functions of vertex position in the scene. | ||
== Light scattering at dawn / dusk == | |||