The observed albedo over a natural water surface, as a function of solar elevation and cloud cover, is reproduced semi-theoretically by considering the distribution of slope on the sea surface. The relation of the albedo to the wind velocity and the turbidity of the atmosphere is also considered.
CITATION STYLE
Burt, W. V. (1954). ALBEDO OVER WIND-ROUGHENED WATER. Journal of Meteorology, 11(4), 283–290. https://doi.org/10.1175/1520-0469(1954)011<0283:aowrw>2.0.co;2
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