Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 2
A persistent weak layer (PWL) of faceted snow exists on northerly-facing slopes at mid and upper elevations. This layer has the potential to produce avalanches ranging from 1 to 3 feet deep and over 100 feet wide. Recent avalanche activity and field observations indicate that slopes most prone to sliding are those that have been recently wind-loaded or have a slab of stronger snow overlaying the buried PWL (see video).
Although the PWL is present at both mid and upper elevations, as we move further from the most recent notable loading event and experience additional days of warm weather, the likelihood of triggering an avalanche on this layer at mid-elevations has decreased. However, the layer still exists and will become problematic again with additional loading.
Be cautious of westerly, northerly, and southeasterly facing upper-elevation slopes, which have received the most wind and snow and where temperatures have remained cooler.
Video: Greg Gagne explaining the snowpack structure.