Opposition effect is a nonlinear increase in the brightness of an object cl
ose to astronomical opposition. We present a comparison and summary of the
phase curves of some icy solar system objects, and terrestrial ice. We have
constructed a method of approximating the height and width of the oppositi
on peak and evaluating the practicality of the method in each case, with th
e aid of a four-parameter fit to a linear-exponential function and computin
g the a posteriori probability distribution of the height and width of the
opposition peak. The procedure described is most applicable in finding a re
alistic fit and evaluating the suitability of data, even with moderate inac
curacy. We have studied the effect of the number of data points to the feas
ibility of the fit, in order to estimate the minimum amount of data require
d for a desired accuracy. Furthermore, we present an interpretation of the
phase curves by means of two scattering mechanisms with important applicati
ons to the recent study of the opposition effect: shadowing and coherent ba
ckscattering. (C) 2001 Elsevier Science Ltd. All rights reserved.