Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
Once initiated, a fresh drift like the one pictured above, may break into weaker layers of the snowpack as it crashes down on the slope below, triggering a slide that gets quickly out of hand.
Winds have been blowing for days and there's no shortage of fresh snow available for transport. Problem is... newly formed drifts conceal older wind drifted snow that formed early in the week. So, yes... the entire deal is a bit more complicated than meets the eye. In addition, the snowpack has gained a substantial amount of buoyancy and will feel strong and solid underneath us. But remember- hard, dense snow can give us a false sense of snow stability, allowing us to get out further onto a slope before it fails and brings the entire roof down on top of us. Found mostly on the leeward side of upper elevation ridges, due to the strength and duration of winds, I'd also be on the lookout for fresh drifts around terrain features like chutes and gullies. In either case, both new and older drifts now rest on weak, faceted, older snow and that means avalanches are gonna be easy to trigger.
Obvious signs of unstable snow include cracking, collapsing, and whoomping noises as well as natures freebie... natural avalanches!