Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Unlikely
- Größe
- 2
There is a widespread persistent weak layer (PWL) of faceted snow on northerly-facing slopes at the mid and upper elevations. On some upper-elevation slopes, there is a stronger slab on top of the PWL where it is possible to trigger an avalanche. We have not received any observations from the Provo mountains in over a week, but observers in the Salt Lake mountains have also noted the entire snowpack is now nearly all facets:
Sam Kapacinskas in Catherine's Pass
Our locator rose shows where this PWL exists: mid and upper elevation aspects facing northwest through northeast, including upper-elevation aspects facing west through southeast. A common theme from the three observations is that, although the PWL is present, it is currently not a widespread problem as we lack a slab on top of the facets, but with heavy, dense snow and strong winds forecasted, expect a rising avalanche danger as we place a load on top of this PWL.