Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1–2
The wind has been transporting snow above the rain/snow line these past few days at Snoqualmie Pass building Wind Slabs, and more recently at all elevations. Public observations on Tuesday confirm that multiple D2 Wind Slabs were triggered by humans within the Snoqualmie Pass zone, so keep them on your radar heading into Wednesday. Wind Slabs often develop on leeward slopes, at the base of cliffs, or on the sides of gullies, but you can look for fresh cornices, textured surfaces, or smooth pillow-like piles of snow to help you determine more specific locations to avoid. As you ascend in elevation above the previous rain line from this weekend, slabs could be much larger and possibly more reactive. Take note of clues of unstable snow such as shooting cracks or whumpfing collapses as you travel, and use small test slopes to test for slab potential and poor reactivity. If you notice any of these signs of instability, steer around wind-loaded slopes.
(12/22/2020) This Wind Slab was human triggered on Tuesday on a common ascent route in the Alpental Valley.