A. Macke et al., THE INFLUENCE OF INCLUSIONS ON LIGHT-SCATTERING BY LARGE ICE PARTICLES, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 101(D18), 1996, pp. 23311-23316
The scattering of visible light by ice crystals containing scattering
and absorbing inclusions is calculated by a combination of ray-tracing
and Monte Carlo techniques. Results are shown for a randomly oriented
hexagonal ice column containing ammonium sulfate particles, soot part
icles, and air bubbles. It is shown that a noticeable change in the ic
e crystal scattering properties compared to a pure crystal requires ab
out 10(3) to 10(4) internal scatterers of a size comparable to the wav
elength. While the nonabsorbing ammonium and air bubble inclusions gen
erally decrease the asymmetry parameter g, soot provides a strong incr
ease in g caused by the additional absorption. An independent superpos
ition of the scattering properties of ice crystal and inclusions does
not give satisfactory results because of the strong influence of inter
nal scatterers on the characteristic ray paths inside the crystal. Mul
tiple-scattering calculations show that the strongest changes in the r
adiative fluxes are associated with the soot contaminated ice crystals
.