Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
Our persistent weak layer (PWL) of faceted snow that formed during the mid-November drought is buried underneath 2-4' of snowfall and wind-drifted snow and avalanches failing on this buried PWL were last reported over a week ago. On my field day yesterday, my partner and I were focusing at the mid-elevations and were finding the PWL continues to slowly gain strength (video discussion below). UAC director Mark Staples was in Pink Pine yesterday and was also finding increasing stability on slopes with the PWL.
Although we are moving in the right direction, spatial variability exists and human-triggered avalanches are possible, especially on slopes that were wind-loaded during the strong wind event from this past Wednesday and Thursday.