Abstract
Abstract The albedo of the whole earth is calculated to be 35 per cent, largely on the basis of Danjon's visual lunar measurements. The calculations also give a value of about 0.50 for the average albedo of clouds, which is in better agreement with measurements than the currently accepted value.
Cite
CITATION STYLE
APA
Fritz, S. (1949). THE ALBEDO OF THE PLANET EARTH AND OF CLOUDS. Journal of Meteorology, 6(4), 277–282. https://doi.org/10.1175/1520-0469(1949)006<0277:taotpe>2.0.co;2
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