Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 3
The situation is very simple - there is a persistent weak layer (PWL) of faceted snow from roughly 16 days of clear and cold weather in November that now has 1-3' feet of snow on top of it. Over the last few days, this layer has begun producing both small and large avalanches. As we continue to add more snow, and more wind to this weak layer we will only continue to see larger and more destructive avalanches occurring.
- We've found buried soft sugary snow at all elevations and on slopes facing every direction. The persistent weak layer (PWL) problem has the potential to get worse as widespread slopes with poor snow structure are overloaded, and the problem is likely to be an issue for a while.
- Areas plagued by a very sensitive PWL consisting of buried feathers of surface hoar are also widespread, but we've found them mostly in sheltered low and mid-elevationon terrain. Persistent weak layers consisting of surface hoar are notoriously tricky, often surprising and sometimes catching experienced avy pros off guard. Avalanches failing on buried surface hoar may occur on lower angled slopes than you might expect.
- Red Flags indicating PWL instability will include audible collapses or wumpfs and shooting cracks. Slab avalanches failing on a buried persistent weak layer are likely to be remotely triggered from a distance, hopefully from above or from an adjacent slope, and not from below.
Monday's snow fell on bare ground or very shallow snow on low and many mid elevation sunny slopes, (W, SW, S, SE) so the danger of avalanches is lower (Moderate), but potential might be higher for hitting rocks.
Video from our field day yesterday near White Pine Knob where we were able to find the weak faceted snow beneath the recent snowfall.