Wind Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible - Likely
- Tamaño
- 1–2
Up to 10 cm of fresh snowfall, and 10-20 cm of low density snow from the previous storm has been redistributed by strong southerly winds, forming reactive windslabs in leeward terrain.
Older, larger, firmer windslabs sit on top of the mid February rain crust on most aspects. Deeper avalanches failing at this layer are less likely, but could have more serious consequences. Larger triggers like cornice or ice falls have the potential to trigger deeper windslabs.
The most likely place to trigger a wind slab is near ridge crest and on convex terrain features. Use extra caution when dropping into a run, highmarking, or travelling on ridges.