Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 1–2
Multiple slab avalanches were reported following Tuesday's storm. They failed on weak snow that developed at the surface during the drought of January and early February. Check out Chris' video (at right and below) for an idea of what we're dealing with.
The majority of these slabs occurred on shadier aspects between 8,000 and 8,500'. This band seems to have the ideal combination of slab formation and a well-preserved weak layer. Why? It stayed mostly dry; high enough to escape much of the rain, and shaded enough to avoid melting in the sun. It's protected. This band is near the upper/middle elevation transition, so it's just low enough to avoid being heavily weathered by the wind.
These are not your more predictable, run-of-the-mill wind slabs. You can't simply look for and avoid areas of wind-drifted snow. These avalanches are likely to behave in ways that surprise you. They can wrap around terrain features like ridges and may be triggered from flatter terrain below, above, and to the sides of steep slopes.
ADDITIONAL DISCUSSIONCloud cover and cooler air will reduce the chance of wet snow avalanches. That said, the snowpack will take a bit of time to solidify after days resembling a bowl of oatmeal. If the sun peaks through the clouds, it won't take long to break down any surface crusts that formed last night. If you're sinking into slush, find gentler terrain or cooler slopes to ride.