Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2–3
Buried weak layers of facets and depth hoar sit near the base of the snowpack. These layers were responsible for the last slab avalanches reported in this zone (see photo) and remain our greatest concern. Triggering an avalanche on one of these layers is unlikely but the resulting slide will be massive. Unfortunately, knowing exactly when or where you’ll trigger one of these beasts is impossible to tell.
Dealing with this problem is an odds game. Here are some considerations to help you reduce your risk:
- Wind-loading: Slopes with stiffer snow near the surface–whether from wind-loading or "spin drifting" below large cliff faces–are more likely to produce big avalanches than areas where the surface is loose powder.
- Likely trigger points: You are most likely to impact the deeply buried weak layers on parts of a slope where the snow cover is thin, like near rocky outcrops. Heavily wind-affected areas where the wind created a complex pattern of scoured and loaded slopes are also more likely to be problematic.
- Slope angle: Avalanches are most likely in "prime time" avalanche terrain, slopes around 35-45 degrees in steepness. However, remember that persistent slab avalanches can be triggered remotely–from gentler terrain below or to the sides of steeper slopes.
Additional Discussion:Yesterday, skiers in the Sawtooth Mountains found touchy wind slabs at upper elevation. Be alert to similar conditions today as W and NW wind forms drifts in exposed terrain. If the clouds hold off until later than forecast, loose snow avalanches are a possibility again this afternoon. These slides are most likely on sheltered SE-S-SW-W facing slopes while they directly face the sun.