Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2
The recent storm began with strong southwest winds which shifted to the northwest later in the day and continued to blow overnight. Mountain topography can cause strong winds to swirl and change direction loading any aspect. With plenty of low density snow available for transport, expect to find unstable drifts in unusual places. Wind slabs will be further down off the ridge lines than you might expect and on mid-slope terrain features. Below treeline terrain even gets in on the action today. Use caution while exiting drainage bottoms and avoid terrain traps.
Wind drifted snow is stiffer and more compact than non-drifted snow. Cracking and collapsing is a sure sign of instability. This problem is most pronounced near treeline and above on slopes with a northerly and easterly component to their aspect.