Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Since the recent low pressure system passed on Thursday night, we have been having pretty ideal weather conditions for the healing of our wind slabs- moderate warmth and light winds. Touring around Tam Rim on Saturday, snowpack tests confirmed trending stability, and I did not encounter any reactive wind slabs. That being said, I'm not quite ready to remove this problem completely, and the colder temperatures at upper elevations have likely slowed the stabilizing of these slabs. It is at these above treeline elevations on leeward terrain (NE - SE) that I would expect it is still possible to trigger a wind slab avalanche.
Isolated terrain features have the potential to produce large avalanches. Steep and unsupported terrain are the slopes where avalanches are more likely to be triggered. Utilize snowpack testing such as hand sheer tests to gain a better understanding of the presence of slabs. Additionally, safe test slopes can be a great indicator that wind slab avalanches could happen on similar terrain.