The remote sensing reflectance, which is defined as the water-leaving radiance to the downwelling irradiance, is commonly used in ocean color remote sensing, but the water albedo theorectically conveys more information about waters since it is the hemispherical integration of remote sensing reflectance, why the ocean color community uses remote sensing reflectance rather than water albedo? Is there any hard nut to crack in the observation of water albedo?

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