Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Unlikely
- Größe
- 1–2.5
Recent observations show that our PWL (Jan 31 buried facet layer) appears to be gaining strength, or 'rounding'. Stability tests on this layer show promising results for this trend, but the weak layer (and therefore weak snowpack structure) is still present in specific locations, even though it is becoming more stubborn to trigger an avalanche. Bear in mind that Persistent slab problems are notorious for having wide spacial variability, and certain terrain features (e.g. convex slopes and shallow rocky areas) could see a greater likelihood for triggering an avalanche on this PWL. With this stabilizing trend we will be less likely to get our typical red flags like collapses and whumphs, even when a reactive slab is present. Patience and continued caution remains necessary. If a Persistant slab avalanche were to trigger, it could result in a large, potentially fatal slide.