Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1
If you can trigger any avalanches, it is probably in newly formed wind slabs at upper elevations. Upper elevations received a foot or more of snow in the last week. Depending on how far up you go, the snow will become increasingly dry. Any low-density snow will have recently been redistributed into wind slabs.
Relatively warm temperatures mean any weaknesses will probably strengthen quickly, but there's a tiny chance you could still trigger a slab avalanche in a newly formed slab. Identify wind-loaded stiffer slabs in areas such as around features, along ridges or sub-ridges, and in gullies. If you have any doubts, avoid these wind slabs on steep slopes.
Example photo: A human triggered slab avalanche. Signs of wind loading are the scoured snow on the ridge just above the crown and the cornice in terrain above. An old rain crust is visible in the bed surface. Northwest aspect at 5100'.
Photo: NWAC Public Obs