Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 1–2.5
As snowfall increases during the daytime, storm slabs should become more reactive. These could break within the storm snow, at the old snow interface, or even deeper on a number of weaker layers. The new snow is covering up a previous surface of facets and surface hoar. As such, slides may fracture widely or be triggered from adjacent slopes. They could be even be triggered in sheltered terrain once enough new snow piles up. Above 5,000ft slides could run on more deeply buried weak layers including weak snow and a crust from early February, and they could be over 2.5ft deep in places.
With these dangerous conditions and snowpack complexity, it'll be a day to keep it simple with your terrain if you decide to venture out. Avalanche danger is expected to continue increasing into the overnight period, so it won't be a day to hang it out there.
Example storm slab in terrain below treeline.