Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 4
We can expect more of this today. The avalanche on this upper elevation northeast facing slope was initiated by a small piece of snow releasing on a steep, rocky face near the ridge, which then triggered a much larger slide as it crashed onto the slope below.
A persistent weak layer (PWL) of weak, faceted snow is buried 1-3 feet deep. It's hard to believe that this layer is still alive and well, lurking in the snowpack, despite such warm weather. When you see it and feel it, it's almost shocking how dry and loose it is (like a layer of shugga... baby :). The snowpack continues to show us that this layer will fracture and produce avalanches.
Where does it exists? It is widespread on NW-N-NE-E facing slopes near and slightly below treeline. Above treeline in alpine terrain, it's distribution is more pockety.
What will the warm weather do? For now, "all bets are off" and conditions remain dangerous. In the long run, the warmth will help this layer slowly heal. The wild card is that if there's enough heat to melt snow and cause liquid water to percolate down to this layer, then avalanches would start happening on their own.