Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–1.5
New snowfall and a wind direction of W-SW blowing at moderate to strong speeds will develop drifts on north, east, and south aspects. This will cause stress on a pre-existing surface crust that could serve as a bed surface and a weak layer. As surface slabs build, the soft snow beneath will make for an unstable snowpack structure. If the storm comes to fruition, snow totals could reach double-digits. This will cause drifts to grow in size and sensitivity as the day advances. Five inches of snow could translate to a foot or more of drifted snow in specific areas. By monitoring the depth of slab growth and how reactive it is, you also monitor the increasing potential for danger. Risky locations include the sharp, leeward sides of ridgelines and the pockets of cliffs and gullies. By identifying where blowing snow is occurring and using clues like, fresh wind lips, snow texture, and pillow-like surfaces, you can better gauge where wind-deposited snow may be lurking.
(1/10/2024)
Wind transport and active snowfall rapidly accumulating on the leeward (left) side of the ridge.
Photo: Eric Falconer