Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1.5–3
Snow and an overall warming trend will likely make a weak layer of surface hoar that developed late-January reactive to riders. Prior to this storm, the layer was found 15 to 60 cm deep across the region, being deepest in the south and shallowest in the north. This layer has been the most sensitive right at treeline, but it may extend up into the alpine, and be found in openings in the trees below treeline. The likelihood of triggering this layer is expected to increase once a cohesive slab develops above it.