Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Unlikely
- Dimensione
- 3
Several feet of snow, containing over 6 inches of water, should eventually help heal our persistent weak layer (PWL) problem. However, for now, it has only complicates the situation. What was once a 1-2' slab in early February has now transformed into a 3-6' slab throughout the range, potentially even deeper in wind-drifted 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.
The weak layer is just as strong as it was prior to the storm, but now the slab over the top is significantly thicker. The bottom line is that there's more weight, resulting in larger avalanches. It's imperative to give this weak layer time. While the new snow instabilities should be settling, there may still be some sensitive soft slabs across all aspects and elevations in the range. Any avalanche initially triggered in the new snow could potentially step down deeper in areas where the persistent weak layer (PWL) is known to exist.