Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 2
Persistent weak layer problems remain on northerly aspects above treeline where old hard slabs of wind drifted snow sit on top of underlying weak facets. The primary layer of concern is a layer of facets that formed near the surface before the storm on January 23. Several windy periods since have built stiff hard wind slabs over top of this faceted layer and human triggered avalanches 1-2 feet deep are possible. A less likely, but not impossible scenario would be for an avalanche failing on this weak layer to step down deeper into the snowpack. For these reasons, I'm still leery of upper elevation, wind loaded terrain. Avoid steep slopes just below ridge lines that have smooth, hard slabs of wind drifted snow or that sound or feel hollow underneath.
Looking ahead, any significant snow load, especially if combined with wind, will have the potential to produce large avalanches breaking below the Christmas rain crust and taking out the entire season's snowpack.