Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Strong E-SE winds, particularly near the Cascade crest, formed slabs in some unusual locations and aspects earlier this week. In the Crystal backcountry, several small avalanches were observed Thursday by an NWAC forecaster. These slides were around 8” thick on SW facing slopes. Look for subtle clues such as small drifts and changes in the feel of the snow underneath you to locate wind affected slopes. You may find wind slabs well below ridgelines and along the sides of cross-loaded gullies and features. Some of these slabs may be more than a foot thick and could produce avalanches large enough to bury you. If you suspect wind loading on a slope, go around and seek out less wind-affected or lower angled terrain.
We continue to find evidence of buried persistent grains in the Crystal area. We are uncertain if a similar snowpack structure exists in other parts of the zone. If these wind slabs fail on facets, surface hoar, or crust/facet layers they may produce surprising avalanches that trigger easily, propagate widely, and run quickly.
(1/28/2021) This small slab avalanche occurred well below ridgeline on East Peak Thursday. Other similar slides were observed later in the day.