Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1–2
Increasing southwest winds are drifting recent snow into slabs on leeward-facing terrain. Slabs will become thicker and more widespread as you gain elevation. An avalanche in the wind-drifted snow can step down to a buried weak layer resulting in a much larger slide. Look for blowing snow as you climb in elevation and note the density change in the snow you are traveling through to identify a slab. Cracking in the wind-drifted snow is a sign of instability, directing you to seek safer conditions in sheltered terrain.
(1/1/2023)
A well-developed cornice line from southwest winds cross-loading mid-elevations.
Photo: Mark Dundas