Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2
The persistent weak layer (PWL) dominating much of the snowpack on north-facing slopes continues to lose strength. As new snow or wind arrives, this weak structure will struggle to support additional weight and may begin to collapse. Take note of which slopes, aspects, and elevations are or are not holding snow, so you’ll know which areas to avoid during the next storm.
Weak snow is also forming on the surface and you can learn more about surface hoar HERE. The question is whether or not the warmer temperatures and wind will destroy this surface weakness before it snows?