Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
The recent snow is very low density and will be easily moved by the wind. Even with light winds in the forecast, we could see some significant drifts. Below ridges and highpoints are places where wind blown snow often accumulates. Slabs can also form as wind moves across a slope and fills in depressions and gully features. Wind slabs can be tricky to judge because some lee features will have minimal wind loading while other features seem to collect a lot more blowing snow. Deeper wind deposits can lead to larger avalanches. The wind direction may shift around the compass on Thursday, hence the distribution on all aspects.
Archive Photo:
Cracking in wind drifted snow. This is a classic indicator of unstable snow.