Wind Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Likely
- Tamaño
- 1–2
With moderate to strong winds, wind slabs can form in weird places and in some cases not at all. Sometimes the blowing snow blasts into the atmosphere never to be seen again, and in other cases it can create deep wind slabs on certain terrain features. Nature can be unpredictable, but we can look for where blowing snow is ending up and look for signs of wind slab formation.
Wind slabs typically form below ridge tops, high points, and terrain features that catch blowing snow. If you can judge that a slope has not been wind loaded, then a wind slab is not a problem.
Watch for signs of blowing snow to indicate slopes are becoming loaded. Look for visual clues on the snow surface, such as pillowy deposits and wavy or ripply surface texture, to let you know if previous wind transport has occured. Wind deposited snow can be many times deeper than the snow the storm has dropped out of the sky.
As drifts become deeper, resulting avalanches can become larger. Ease into terrain by checking out the wind loading on lower angle slopes. Monitor the depth of wind slabs and look for signs of unstable snow.