Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
There is weak, sugary faceted snow (a persistent weak layer, or PWL) buried 1-4' deep on almost all aspects and elevations throughout the Wasatch Range. Avalanches on this layer are most likely on slopes facing northwest-north-east-southeast.
Today, the likelihood will be especially prominent on any slopes that receive the additional weight of wind-drifted snow. For the snowpack, when the winds drift snow, it's the same as if snow is falling out of the sky. The snowpack doesn't care where the snow comes from, it feels the added weight. So, on northerly-facing slopes, these winds have added snow and weight, and stress to the persistent weak layer. Outside northerly-facing terrain, with the additional load of wind-drifted snow, we may begin to see activity on aspects and elevations that have been quiet over the last few days.
Avalanches are unlikely on solar aspects west through south where there haven't been any reported avalanches on this layer. The easiest way to avoid any avalanche is to go on slopes less than 30 degrees with nothing steeper above. Read about slope selection HERE.