Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1
By mid afternoon wind slabs may develop enough to elevate the avalanche danger. New snow will be very obvious on most aspects, where a crust formed on the surface over the last couple days. On upper elevation northerly aspects finding the new/old snow interface will prove more difficult, as that area didn’t previously have a surface crust. You could find the change by digging with your hand down into the new snow and identifying a difference in appearance or texture between the two layers. In those areas wind slabs may slide easily, as there are reports of weak snow developing at that surface in the last two days. Fresh wind deposits might also slide easily on the slick crust on other aspects.
Search for pockets of recently drifted snow by identifying fresh pillows of snow or textured surfaces. They are most likely to form in gullies, beneath cliff bands or around features. In areas where the deposits are greater than about 6 inches consider avoiding steep terrain, as these may be large enough to take you for a ride.
An example of a recent 6 inch skier triggered wind slab. This is similar to what you may find by the end of the day on Wednesday.