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. DOI: 10.1103/PhysRevLett.117.096101 Nakaya summarized his research on snow flakes in a famous haiku: "They are letters sent to us from the sky" [1]. Indeed, the habit of ice crystals grown from bulk vapor change from plates, to columns, to plates, and yet back to columns as the temperature is cooled down below the triple point, with the well known dendritic patterns appearing at sufficiently high supersaturations [2]. Accordingly, the final growth form of a tiny ice crystal conveys detailed information on the atmosphere where it grew [3].At a macroscopic level, it is well known that changes in ice crystal habits result from a crossover in the growth rates of the basal and prismatic faces, but exactly what structural transformations occur on the surface to drive this crossover is far from being understood [1,2,4,5]. Kuroda and Lacmann explained the crossover in crystal growth rates as a result of the formation of a thin quasiliquid layer on the ice surface that could set up at different temperatures depending on the crystal facet [6].The hypothesis that ice could exhibit a quasiliquid layer dates back to Faraday, and the formation of such a layer on solid surfaces is now well characterized theoretically as a premelting surface phase transition [7]. Experimentally, the advent of modern optical and surface scattering techniques has allowed us to gather ample evidence as regards the existence of a premelting liquid film on the surface of ice [8][9][10][11][12][13][14]. Unfortunately, the relatively high vapor pressure of ice makes it very difficult to achieve sizable equilibrium crystals [2], while the presence of impurities has a very large impact on the surface structure [12,15]. Accordingly, many other relevant properties, such as the premelting temperature, the thickness of the quasiliquid layer, or the presence of surface melting remain a matter of debate [8].One particularly important structural property with a large impact on crystal growth rates is the surface roughness [6,16,17]. Contrary to smooth or singular facets, which have a limited number of defects and serve as the basis for most crystal growth models, rough surfaces present diverging height fluctuations, which do not differ macroscopically from those found in a fluid interface. As a result, rough crystal planes with correlation lengths that are larger than the crystallite disappear and become round [18][19][20]. More importantly, as far as the crystal habits and growth forms are concerned, the roughening of a s...