Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 3
Several feet of snow, containing multiple inches of water, should eventually help heal our persistent weak layer (PWL) problem. However, for now, it has only complicated things. Whereas on January 31st, you could find a 1-2 foot slab on top of the facets (the PWL) in thinner snowpack areas, there is now an additional 2-3 feet of snow on top of the PWL, and even more in the wind-loaded areas.
The likelihood of triggering an avalanche on the PWL is very low in the Ogden area, and I would almost describe the PWL as dormant. However, with the addition of water weight over the past few days, we aren't ready to put the layer completely to bed yet.
UAC forecaster Dave Kelly perfectly describes the situation in his field day on Thursday in Days Fork. "The weak layer is no less strong than it was a week ago, but the slab over the top is much thicker. The bottom line is that the difference is more weight. The avalanches will be bigger. Give this weak layer time."