Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
The image above illustrates our setup... notice the smooth texture of the new snow on top of rough, granular looking weak snow underneath.
Now... here's what's going on. The midwinter drought of January and February created a persistent weak layer (PWL) of sugary facets on the snow surface which was buried by last week's light snow. Despite record breaking heat last week, the sugary layer remains cold, dry, and weak. The combo is found on mid and upper elevation slopes facing the north half of the compass along with a sliver of southeast facing terrain. This is our new problem child, especially where a cohesive slab rests on top. Mark commented... "To be honest, it's hard to believe how dry and weak this layer is until you see it and feel it with your own hands."
Here's where it gets tricky... large swaths of upper elevation terrain facing the north half of the compass were blasted by the winds prior to our recent storms and weak snow distribution is spotty at best. That means you'll need to evaluate each slope on an individual basis.