ice from the ultraviolet to the microwave have been given in Warren and Brandt
(2008). The change in the m ref,i with wavelength for water ice at visible wavelengths
is particularly striking but should not be surprising because, as we have noted before
Fig. 4.9 The single scattering albedo for four different values of the imaginary part of the refractive
index. Solid: (1.60, 0.1); Dashed: (1.60, 0.01); Dot-dash: (1.60, 0.001); Dot-dot-dash: (1.60,
0.0001)
Fig. 4.8 Definitions of regimes for the single scattering albedo as a function of the size parameter
(following Moosmüller and Sorensen 2018)
4.2 Scattering of Light by Dust
293
(2008). The change in the m ref,i with wavelength for water ice at visible wavelengths
is particularly striking but should not be surprising because, as we have noted before
Fig. 4.9 The single scattering albedo for four different values of the imaginary part of the refractive
index. Solid: (1.60, 0.1); Dashed: (1.60, 0.01); Dot-dash: (1.60, 0.001); Dot-dot-dash: (1.60,
0.0001)
Fig. 4.8 Definitions of regimes for the single scattering albedo as a function of the size parameter
(following Moosmüller and Sorensen 2018)
4.2 Scattering of Light by Dust
293