Cornices
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1
Again last night, air temperatures were well above freezing at the mid and upper elevations. A decent overnight snow surface refreeze is expected to have occurred due to radiational cooling under clear skies despite above freezing air temperatures. As daytime warming progresses, isolated areas of minor wet snow instability may form on a variety of aspects. Areas near exposed rocks that act as heat sinks and in gullies that focus parabolic reflection onto the snow surface will experience greater snow surface melting. These areas will also be the most likely places for a small human triggered wet snow instability to occur. On northerly aspects, slab avalanche activity remains unlikely today. Weak snow that exists near the snow surface in many areas generally lacks a sufficient overlying slab. Exercise normal caution and keep an eye out for potential isolated areas of localized instability.