Wind Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Likely
- Taille
- 1–2
As the temperature drops, new incoming snow will be low density by Central Oregon standards and easily moved by the wind. Wind slabs forming over unconsolidated snow will be especially sensitive to triggering. The potential for wind slab avalanches to become large exists in select pockets of terrain.
Wind slabs often form below ridge tops, high points, and around featurs that catch blowing snow. Look for visual signs such as pillows of wind difted snow, and a wavy or uneven surface texture to indicate a surface may be wind loaded. Recently formed cornices can also be clues that wind slabs are present.
If you encounter signs of windloaded snow or observe cracking in the surface slab, move to lower angle slopes under 30 degrees.