An empirical model has been found with which to calculate depth profiles of the mean cosine of a component of radiance in homogeneous water under a flat surface. Model inputs are the refraction angle ω′ and the subsurface downwelling irradiance Ei due to the entering radiance component. Other inputs are the absorption and scattering coefficients, a and b, and the angular scattering function (here Petzold’s functions for San Diego Harbor or “Tongue of the ocean” Atlantic waters). The model applies to refraction angles up to 48° and b : a ratios up to 20. Model profiles of the mean cosine match Monte Carlo profiles to ±0.01. From mean cosine profiles, scalar irradiance profiles are calculable; down to the 1% light level, model and Monte Carlo irradiances agree within ±10%. The time to compute an irradiance profile with the model is ∼ 10−4 that of a Monte Carlo calculation.
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T. T. Bannister (1992) studied this question.
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