Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 2
The underlying snow pack is weak, but the December drought layer (buried roughly 15 inches deep) is the primary layer of concern. This layer of weak, faceted snow formed near the surface during the December dry spell. A slab now exists on top of this persistent weak layer. Near treeline and below, storm snow over the past week has settled into a thick, cohesive slab. Near treeline and above, elevated winds have stiffened the snow and produced slabs of wind drifted snow over top of this weak layer. This persistent weak layer is most widespread on slopes facing W-N-E, but faceted snow is turning up on all aspects, and it may only be a matter of time before we consider this problem to be widespread.
The video below of an extended column test illustrates the slab's ability to propagate and produce an avalanche: