Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2.5
Recent snow and strong winds have created wind slabs at middle and upper elevations. In areas exposed to the wind these slabs will be stubborn or even scoured to the hard bed surface. In more wind sheltered areas, the slabs are likely to have retained the structure needed to propagate and fail as a slab avalanche. The largest wind slabs will be found in east facing ravines at middle and upper elevations. Observers yesterday noted large slabs formed higher up in the start zones of south and southeast facing avalanche paths including the south facing gullies of Tuckerman Ravine.
In the last 48 hours, the snow surface has been affected by strong wind loading snow, wind scouring snow and also sun warming south aspects. What remains is a highly variable snowpack which will feel and act differently by aspect and elevation. Evaluate the snowpack carefully and continually in avalanche terrain today to eliminate the chance for surprises.