Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Yesterday, riders in the Baker Creek drainage triggered two avalanches on upper elevation, wind-loaded slopes. They both broke over 100' wide and 12-16" thick and occurred on E-NE aspects near 9500' (photo, photo). While multiple weak layers exist in the upper portion of the snowpack, a thin layer of facets atop a crust is emerging as the top contender. This persistent weak layer seems most prominent on mid and upper elevation slopes facing E-NE-N-NW, although uncertainty exists regarding its overall distribution. This layer was responsible for a small skier-triggered slide on Wednesday near the head of Smiley Ck in the W. Smoky Mountains. In the northern Sawtooths on Thursday, I found it buried beneath a 16" thick slab and received unstable snowpack test scores (video above/right).
Slopes having the right (or wrong) combination of weak layer and overlying slab are not widespread. In my mind, this is not a good thing! I would rather have unstable conditions nowhere, or everywhere. The spotty nature of the problem makes assessing each slope you want to ski or ride a gamble, and conditions are ripe for getting surprised.
You are most likely to trigger a persistent slab avalanche in upper elevation/alpine terrain where the wind has redistributed snow and formed a thicker slab atop the weak layers. But it's also possible to trigger one on wind-sheltered slopes with "prime-time" slope angles steeper than about 35 degrees. The best approach is to take a step back and choose more conservative terrain. The safest slopes are those protected from the wind and less than 35 degrees in steepness.
ADDITIONAL DISCUSSION:While cloudier skies are in the forecast today, temperatures will be very warm. It may become possible to trigger small wet slides on very steep (approaching 40 degrees) slopes that face the sun. Pay attention to the tendency for the surface snow to peel away from your skis or sled and slide downhill on underlying crusts.