Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
North outflow winds that occurred for about an 8 hour period on the evening of the 15th through the early morning of the 16th have come to an end. Winds have already switched around to the South with the approach of the next weak system. Wind slabs up to a foot in depth formed during this period in specific areas and will be our main concern today. The sensitivity of these will be decreasing from yesterday but will still be possible for a person or machine to trigger. Light snowfall today is not expected to increase the avalanche hazard.
Watch for signs of previous wind loading like textured snow surfaces, and fresh windlips that will point towards wind loaded slopes. Wind slabs are easier than other avalanche to avoid because they can be visually identified unlike persistent slabs and they only exist in specific areas unlike storm slabs. Wind slabs often have a rounded pillowed look, or may have a rippled texture. Using small inconsequential wind loaded test slopes is a good way to test the sensitivity of this problem. Look for cracking on these test slopes that would indicate wind slabs would have the energy to produce an avalanche on a larger slope.
There is a small chance that wind slab avalanches could step down to deeper layers in the snow in isolated areas and create very large avalanches. (see problem2)
Flagging off high elevation ridges near Thompson Pass the evening of the 15th
Photo: Gareth Brown