Abstract. When wind blows over dry snow, the snow surface self-organizes into bedforms such as dunes, ripples, snow-waves, and sastrugi. These bedforms govern the interaction between wind, warmth, and the snowpack, but thus far they have far attracted few scientific studies. We present the first time-lapse documentation of snow bedform movement and evolution, as part of a series of detailed observations of snow bedform movement in the Colorado Front Range. We show examples of the movement of snow ripples, snow-waves, barchan dunes, snow-steps, and sastrugi. We also introduce a previously undocumented bedform: the stealth dune. These observations show that (1) snow dunes accelerate minute-by-minute in response to gusts; (2) sastrugi and snow-steps present steep edges to the wind, and move by retreating downwind; (3) snow-waves and dunes deposit layers of cohesive snow in their wakes; and (4) bedforms evolve along complex, cyclic trajectories. We use these observations to build new conceptual models of bedform evolution, based on the relative fluxes of snowfall, aeolian transport, erosion, and snow sintering across and into the surface. We find that many snow bedforms are generated by complex interactions between these processes. The prototypical example is the snow-wave, in which deposition, sintering, and erosion occur in transverse stripes across the snowscape.;
