Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Additional snow and wind should help to thicken any pre-existing slabs or build fresh slabs throughout the West South zone. Although the largest and potentially more sensitive slabs could be found on leeward slopes at upper elevations, don’t overlook smaller features well below ridgecrest that are prone to wind-loading. Be leery of areas such as convex rollovers, confined chutes and gullies, or the base of cliffs. Uncoincidently, these are the same areas where avalanches often like to initiate. Take a look for textured surfaces or smooth pillow-like piles of snow to help you identify wind-loaded slopes to avoid. Using uptrack tests or small test slopes as you travel is a quick way to look for potential weak layers or slabs. If you suspect that a slope is wind loaded or find that blocks of snow are failing easily in your tests, head for slopes under 35 degrees.
A poor snowpack structure has been identified in some areas of the zone. More details surrounding this layer are in the discussion below, but you should be aware of the possibility of isolated avalanches breaking in surprising ways.
(1/31/2022)
This small wind slab was intentionally triggered by a skier on a NE aspect around 6300'. The avalanche failed at the new-old snow interface. HS-ASc-R1-D1-I.
Photo: Shane Robinson