Loose Wet
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1
A good snow surface refreeze is expected to have occurred last night due to radiational cooling under clear skies despite above freezing air temperatures overnight at the mid and upper elevations. As daytime warming progresses, most wet snow instability today will present in the form of roller balls and pinwheels. Loose wet avalanches of size D1 (too small to bury a person) could be human triggered in isolated areas of steep terrain. This avalanche problem is most likely on E-SE aspects where a combination of full sun exposure and continuous snow cover exists. This problem is less likely on S-SW-W aspects due to thin patchy snow cover in many areas, but still warrants consideration.