Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Around 10 to 30 cm of recent snow has been blown around by variable wind. This snow may be sitting on top of a layer of surface hoar found at all elevations and on all aspects. On solar aspects, the surface hoar may be sitting on a melt-freeze crust, which is a particularly nasty combination. For now, the recent snow has been touchiest where wind affected. Once enough snow accumulates and forms slab properties, this problem may become widespread. This is most likely to occur first in the snowier spots in the west of the region.