Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
NWAC forecaster Josh Hirshberg was out at Washington Pass on Saturday. In an isolated area above 7000ft, he observed a large collapse in a wind slab overlaying a thin layer of weak snow. We have limited observations on the extent of this problem, but high elevations near steep, rocky ridges are the most probable location. Continued east winds may add depth to these potential avalanches, and they could become quite large. While it has been over a day since the last significant wind event, these snowpack conditions can be slow to heal. As you ascend in elevation and begin to approach wind affected open terrain with sparse vegetation, you can quickly dig down to identify any weak snow layers with stiffer slabs on top. Make multiple observations as you climb and consider using very small, steep, but inconsequential terrain features as test slopes. If you can get a mini slab to break on these test slopes, you should stick to low angle terrain in areas sheltered from the wind. While we're focused on older wind slabs, there is plenty of low density snow to blow around. Pay attention if the wind picks up, and you observe drifting snow. New shallow wind slabs may form throughout the day.
(12/3/2022) Very shallow 2-3" chunks of wind slabs could be initiated on kickturns above treeline. Hairpin valley, SW, 7,000ft. Photo: Josh Hirshberg