  We perform computer simulations of the quasiliquid layer of ice formed at the
ice-vapor interface close to the ice Ih-liquid-vapor triple point of water. Our
study shows that the two distinct surfaces bounding the film behave at small
wavelengths as atomically rough and independent ice-water and water-vapor
interfaces. For long wavelengths, however, the two surfaces couple, large scale
parallel fluctuations are inhibited, and the ice-vapor interface becomes
smooth. Our results could help explain the complex morphology of ice
crystallites.
