Abstract
Aircraft-borne radiometer measurements made within three cirrus cloud layers are presented together with associated in situ cloud microphysical data. The angular variation of the observed shortwave radiances is simulated using a Monte Carlo multiple-scattering model, making use of a number of scattering phase functions, both theoretical and experimental. It is found that, in general, the laboratory-measured phase functions yield the closest agreement with the aircraft radiances. -from Author
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CITATION STYLE
Francis, P. N. (1995). Some aircraft observations of the scattering properties of ice crystals. Journal of the Atmospheric Sciences, 52(8), 1142–1154. https://doi.org/10.1175/1520-0469(1995)052<1142:SAOOTS>2.0.CO;2
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