Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 1–2
Our Persistent Slab avalanche problem will exists on North through East aspects near and above tree line. An overall shallow snowpack has undergone a tremendous amount of faceting over a two week period of high pressure. Wind sheltered slopes near tree line will be fully faceted to the ground with 3mm well developed depth hoar being the major concern. Slopes that saw pevious strong winds from just before Christmas have weak faceted layers underneath hard slabs of varying densities and thickness.
We are extremely well connected and uniform with our weak layers at the moment despite the inconsistencies on the surface. Adding a more uniform slab on top of this structure will increase the likelihood of triggering an avalanche into these buried weak layers. Persistent Slab avalanches will have the potential to be triggered from a distance and from lower angle terrain. These avalanches could be large enough to bury, injure or kill a person, especially as we continue to accummulate more and more snow.
An overall weak shallow snowpack is just missing the addition of a more cohesive slab to produce destructive avalanches.