Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1.5–2.5
Sustained winds up to the 40 mph range will be moving a lot of snow to lee terrain features. With this kind of wind speed, wind deposited snow can show up further down slope and in unusual places. It won't be hard to spot blowing snow out there. The wind wrapping around north and south aspects can cause cross loading. Wind slab avalanches have the potential to be larger compared to what we normally see during storm cycles. Use visual clues such as wavy surface texture and pillowy drifits as an indicator of where this problem is present. Previous avalanches and cracking in wind deposited snow are surefire signs that wind slab avalanches can occur.
Remember, wind can pile up snow many times deeper than the snow dropped by the storm. As wind slabs become deeper, avalanches can become larger.
With wind speeds like this, blowing snow may observed in many areas below treeline and areas of sparse or dead trees below treeline can experience a significant wind effect.
It will be best to avoid wind loaded slopes on Thursday.
Archive photo (Elliott Reed)
Example of shooting cracks in wind drifted snow