Computational results have been obtained for radar backscattering cros
s sections of spherical model hailstones containing air bubbles inside
the surface water or spongy ice layer. The effective refractive indic
es of water-air or water-ice-air mixtures have been obtained using the
Maxwell-Garnett and Bruggeman effective medium approximations. The ra
dar backscattering cross sections have been calculated for a layered s
phere composed of an ice core and water-air or ice-water-air outside l
ayer. The amount of air in a surface layer was varied between 0% and 2
0% by volume. The presence of air bubbles in the surface layer shifts
positions of the backscattering peaks and modifies the backscattered i
ntensities at peak values. The dependence of the backscattering cross
section on the air bubbles volume fraction is stronger at shorter wave
lengths.