Abstract
In the present study, the relationship between clear sky spectral (narrowband) and total (broadband) planetary albedos was investigated as a function of the solar zenith angle, surface type, atmospheric conditions, and spectral response of satellite sensors. A Lambertian wavelength-dependent surface albedo was assumed. The simulations could be useful for sensor selection for optimal information on the total surface albedo.
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© 1987 American Meteorological Society
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Pinker, R.T., Ewing, J.A. (1987). The Relationship Between Spectral and Total Clear Sky Planetary Albedo. In: Liou, KN., Xiuji, Z. (eds) Atmospheric Radiation. American Meteorological Society, Boston, MA. https://doi.org/10.1007/978-1-935704-18-8_29
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DOI: https://doi.org/10.1007/978-1-935704-18-8_29
Publisher Name: American Meteorological Society, Boston, MA
Online ISBN: 978-1-935704-18-8
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