Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 4
Ted discovered this well connected piece of snow on the lower east nose of the Humpy ridge that was triggered in the past few days. More on Ted's insight and travels found HERE
A persistent weak layer (PWL) of sugary, faceted snow is buried 1-3 feet deep. I know... I know... 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 just how dry and loose it is (like a layer of shugga... baby :) But wait... there's more! The snowpack continues to show us that this layer will fracture and produce avalanches.
Where does it exist? 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 if there's enough heat to melt snow and cause liquid water to percolate down to this layer, then natural avalanches begin peeling away from steep slopes. Or maybe we roll up on our sled, skis, or board at just the right moment and we're able to pull the rug out from underneath. In either case... no bueno.