Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 3
Persistent weak layers (PWL) of faceted snow continue to plague the snowpack. The two primary weak layers are one from late Nov/early Dec near the ground, and one from early January in the middle of the snowpack or slightly higher.
The slab on top of these PWLs has been getting thicker and denser as a result of recent snowfall, recent wind and recent warm temperatures. Imagine a building with a weak foundation but we keep adding additional floors on top - eventually the whole structure will collapse. Every slope has the weak foundation. What is different is how many floors are on top of it.
The result of this dense slab is that avalanches are getting bigger both in depth and area. Expect avalanches that can be hundreds of feet wide and 2-3 feet deep.
- Above and near treeline this avalanche problem is widespread.
- Below treeline, the weak layer is widespread but the distribution of the slab on top is more pockety and a little dependent on where winds drifted snow and helped create a more cohesive slab.
What's tricky - the first person to ride on or even near a slope may not trigger it. Instead, it may be the 2nd, 3rd, or even 10th person on a slope who triggers it. Seeing tracks on slope doesn't mean it's safe.
Craig describes this set up in the video below
Photo below from an east facing slope shows that weak, rotten foundation in the snowpack near the ground. All the snow above it is what will avalanche.