Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 2
Soft slabs of recent and wind drifted snow exist on all aspects near and above treeline with the greatest danger existing on steep, northerly facing terrain. Wind drifts are recognizable by their smooth, rounded appearance. They may also feel dense or hollow underneath, and cracking is a sign of instability.
In my travels yesterday, I was able to crack out numerous drifts such as this on all aspects. Terrain features can cause mountain winds to swirl and change direction, and load a variety of aspects. You are likely to find fresh wind drifts on the lee side of exposed ridges and in and around terrain features. Watch for and avoid drifts on gully walls, under cliff bands, along sub-ridges, in scoops, saddles, and sinks.
I also found that the new snow had formed a dense, cohesive soft slab in many areas. Storm slab instabilities typically settle out after a day or two, but utilize test slopes to see how this slab is behaving before committing to steeper terrain.