Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2–3
We have a lot of uncertainty at upper elevations, but it's safe to say that sustained SW winds transported large volumes of snow during the recent storm cycle. These slabs formed within denser snow sitting atop lower density snow that accumulated prior to Wednesday. Slabs may be firm, widely propagating, and easily triggered on or under steep slopes. Give these thick slab layers time to heal and any potentially wind-loaded slopes a wide margin of safety. Look for signs of wind affect including recent drifts, wind lips, and firm or punchy snow layers. These could be present at any elevation given plentiful evidence of large wind drifts even in the Methow Valley. Avalanches could run on or step down to older layers in the top 3 feet of the snowpack, especially on steep SW-S-SE aspects. Such avalanches could be very large with low chances of survival.
(1/7/2022)
Example: This very large avalanche was triggered by explosives on 1/7. The very deep (4-6') and wide (500ft) failed on an old snow layer, grew very large (D4) and broke trees. HS-AE-R4-D4-O, NE, 6800.
Photo: Crystal Mt Ski Patrol