Wind Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–2
Cold, weak snow overlaying last week's melt-freeze crust has caused the Wind Slab problem to linger longer than we would usually expect. For the most part, these Wind Slabs are very shallow, but isolated terrain features have produced surprisingly large avalanches like the one Elliott observed yesterday (7,600 NE). If folks are using the good weather to ride higher elevation slopes, it would be wise to make good observations of how deep recently wind loaded snow might be before committing to larger slopes (the melt-freeze crust is an easy landmark in the snowpack).