Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–3
Currently a persistent weak layer is still present in much of our snowpack. These warmer temps will have a positive effect on our deep layer instabilities, but we still need to give it time for bonding to occur underneath the insulating denser slab. Snow pit tests are still indicating weak layer facet instability. Warmer temps could pose as a threat for the time being, giving a false sense of confidence that the facets have been "healed". Continue to give avalanche terrain, especially with terrain traps and higher consequences the margins it deserves.