Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Strong westerly ridgeline winds are drifting recent snow into reactive wind slabs, particularly at upper elevations and areas near the Cascade Crest with higher storm snow totals. The most likely locations to trigger avalanches will be on steep slopes below ridges or mid-slope features such as convex rolls, which are common trigger points. With wind speeds up to 30mph, you may find wind slabs lower down on the slope than you would typically expect. There is a possibility that wind slabs could step down into deeper buried weak layers. This scenario would produce a much larger, surprising avalanche that could be unsurvivable. This problem is particularly concerning in areas near and around Stevens Pass. Although uncertainty exists, similar conditions could also linger in areas further east. With this increased uncertainty, travel with a conservative mindset and consider wider safety margins.Look for signs of wind slab formation, such as actively drifting snow and textured surfaces. You can also use your probe or pole to feel for stiffer snow over softer snow layers. Cracks that shoot away from your feet or equipment are a sure sign of unstable wind slabs. If you observe these long cracks, use lower-angle routes or move to sheltered terrain.
(2/9/2023)
An intentionally triggered wind slab on a leeward slope from Feburary 9th after a significant storm.
Photo: Matt Primomo