We use a mean-field lattice-gas model to describe the equilibrium ice/
vapor interface. The numerical values of the parameters in the model a
re taken from laboratory experiment and molecular dynamics calculation
s. The model predicts the existence at equilibrium of a layer of admol
ecules at the ice surface; it is only a few molecules thick because of
the very strong water-water interactions. Sharp transitions in layer
thickness occur at well-defined temperatures on each crystal face.