Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 4
With a little thump or a cornice fall, avalanches are still breaking to weak snow near the ground like in the image above from Upper Weber Canyon on Monday.
Sure, the snowpack is getting comfortable in its skin, but we can't forget this basic fact... a persistent weak layer (PWL) of faceted snow near the ground still exists. And while we're headed in the right direction, the PWL hasn't miraculously healed overnight. Here's where it gets tricky... while it's getting harder to trigger a deep, dangerous avalanche, we've gotta remember all the dense heavy, December snow, rests on top of a suspect foundation and today's storm has the potential to bring these weak layers back to life. All we need to do is roll along and knock the legs out from underneath.
Here's where it gets dangerous-
- Once triggered, avalanches may break hundreds of feet wide.
- It may not be the first person on a slope that triggers A LARGE, DANGEROUS avalanche, it may be the second, third, fourth, etc. who triggers it.
- Seeing tracks on a slope DOES NOT mean it's safe.
Slopes loaded by south winds are the exact ones where this weak layer exists. The addition of wind-drifted snow will make avalanches even larger, deeper, and more deadly.
Above, I explain what we're seeing on most low elevation slopes and south-facing terrain that had little or no snow prior to the big Christmas storm.