Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
20 - 30 cm of storm snow now sits atop a preserved layer of surface hoar. In alpine and treeline terrain that has been exposed to more wind, surface snow may be redistributed into wind slabs. These wind slabs have the potential to scrub down to a buried surface hoar layer making for larger then expected avalanches. This is especially relevant at treeline elevations where the surface hoar is likely larger and better preserved.