Wind Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 1–2.5
Storm snow has been redistributed by southwest winds into deeper deposits, primarily found on north and east facing terrain features.
A buried layer of surface hoar is increasing the reactivity and propagation of wind slabs. Avoid sheltered and shaded slopes where surface hoar is more likely to be found. On other aspects, this layer is present as a melt freeze crust which has also produced avalanche activity.