Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Very Likely
- Taille
- 4
The situation is very simple - there is a persistent weak layer (PWL) of old, faceted snow near the ground with 3-10 feet of snow on top of it. This layer has been fracturing and producing large and destructive avalanches over the past week. We have adding two huge stressors to this fragile snowpack in the form of heavy wet snowfall and significant wind loading.
This layer exists on west, north, and east-facing slopes where old snow lingered and weakened in November and was buried by December snowfall. It doesn't exist on south-facing slopes because it melted away in November, and December snowfall landed on bare ground on those slopes. The most likely places to trigger a slide in this persistent weak layer are slopes with some wind-loading especially on more northerly facing slopes with the weakest snow.
Given the new snowfall, elevated winds, and poor snowpack structure I would continue to avoid being on or beneath any steep west to north to east facing terrain.