Loose Wet
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1
As daytime warming progresses, the poor to decent snow surface refreeze that occurred last night will transition from supportable crust to deep wet snow. Partly cloudy skies last night will have limited the potential for radiational cooling. The best snow surface refreeze will have occurred in areas where air temperatures were actually below freezing. Once the surface refreeze melts and the snow surface becomes unsupportable, enough unconsolidated wet snow will exist for human triggered pinwheels, roller balls, and loose avalanches to become possible on all aspects at all elevations.