Based on numerical experiments in which the influence of the depth of the optically active layer on the spectral properties of the water-leaving radiances was studied, estimates for the accuracy of the reconstructed diffuse attenuation index using the standard NASA technique were obtained.
An precision of the chlorophyll-a concentration and the detrital matter absorption coefficient using different algorithms for the Black Sea are obtained on the basis of numerical experiments in which varied the depth of the optically active layers and the its albedo. The numerical experiments compared with satellite observations performed in the deepwater part of the Black Sea in the first half of summer 2000 during the intensive coccolithophorids blooms are in good agreement.
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