Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Strong winds following our most recent storm system created wind slabs on all aspects near and above treeline. While these deposits have largely become unreactive, it may still be possible to trigger an avalanche in areas where slabs rest on weak faceted snow or facet crust combos. Periodic probing may be the best way to search for areas with weaker snow below stronger surface layers. Fresh wind deposits are not out of the question today with increasing winds out of the southwest. Recent high pressure and warm temperatures have decreased the amount of soft snow available for transport, but it will still be prudent to watch for clues like blowing snow, large fresh drifts, and hollow upside-down feeling snow. Be suspect of terrain features that encourage drifting, such as the leeward sides of ridgelines, alpine couloirs, mid-slope convex rollovers, and cross-loaded depressions.