Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 2
It's becoming less likely to trigger an avalanche with each passing day but poor snowpack structure, comprised of a dense slab over weak, faceted snow remains. The faceted weak layer is showing signs of gaining strength, meaning that it's becoming more dense, and stability tests performed near treeline and below are generally non-reactive. This, plus the time that has expired since the last loading event and subsequent avalanche cycle, indicate growing stability. Nevertheless, it's still possible to trigger an avalanche if you find the sweet spot, particularly in steep, rocky, wind affected terrain above treeline that faces NW-N-E.
Looking ahead, the snow surface continues to weaken and this will undoubtedly become a future weak layer when new snow finally comes. The underlying structure will also likely become re-active again.