The amount of solar energy reflected from various soils and types of vegetation has been measured as a function of sun elevation in six different wavelength ranges in the ultraviolet, visible and near-infrared regions of the spectrum. It is shown that there is a significant dependence of reflectance on both wavelength and elevation of the sun for all surfaces for which measurements were made.
CITATION STYLE
Coulson, K. L., & Reynolds, D. W. (1971). The Spectral Reflectance of Natural Surfaces. Journal of Applied Meteorology, 10(6), 1285–1295. https://doi.org/10.1175/1520-0450(1971)010<1285:tsrons>2.0.co;2
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