Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Unlikely
- Dimensione
- 2–3
We've been plagued by persistent weak layers the entire season. First by early-season facets near the ground, then by weak layers that were buried in late-January and February. Warm temperatures and a lack of loading over the past 5 days have finally given these layers the breather they need. Observations from across the forecast area indicate that weak layers are stabilizing. Consequently—for the first time in well over two months—the likelihood of triggering a persistent slab avalanche has decreased to "unlikely."
There are two types of snowpacks in this world: those with persistent weak layers, and those without. Even if both snowpacks are considered "stable", I'd choose the one without weak layers every single time. So even as our snowpack trends towards stability, don't let your guard down. Even though triggering a persistent slab avalanche has become unlikely, that's not the same as impossible. If I had to describe where there's still a small chance of triggering a persistent slab avalanche, it would be on very steep (approaching 40 degrees), rocky, wind-affected slopes. Terrain like this is most common at upper elevations and especially in the alpine.
There's still a small chance of triggering a persistent slab avalanche, primarily in terrain like shown in the photo—very steep, rocky, and wind-affected. Pole Creek area.