Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 3
A persistent weak layer of dry, sugary faceted snow exists on NW-N-NE-E aspects beneath a slab that is 2'-3' thick. The weakest snow exists on northerly aspects right around treeline and below. Above treeline, weak layer distribution is more variable but the problem has been compounded by recent wind drifted snow. Stability tests this week have shown that avalanches were becoming harder to trigger on this weak layer, but that could change with these dramatically warm temperatures. The concern is that melt water will percolate down to these weak, sugary facets, increasing the likelihood for human, or even natural avalanches. In the long run, these warm temperatures will help to consolidate and strengthen the snowpack, but in the short term we are in a tenuous, transitional state.