Loose Wet
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Continued warming today, a poor refreeze overnight, and full cloud cover will continue to warm the snowpack today, possibly leading to a wet loose avalanche cycle. Surface snow consists of up to a foot of weak sugary near surface facets. These crystals can be especially susceptible to rapid warming or “greenhousing” from cloud cover.
If you find yourself moving through wet or unsupportable snow, or see small wet loose avalanches beginning to fan out and increase in size, expect a wet snow avalanche cycle and stay out of avalanche terrain. The timing of wet snow avalanches can be tricky when we are dealing with greenhousing from cloud cover versus wet snow from strong sunlight. Wet snow from the cloud cover will be possible first thing this morning so do not let your guard down as you approach your objective for the day.
At upper elevation this problem will transition into a dry loose problem with sloughing of the near surface facets. It is hard to put a definitive elevation line for this transition and it will likely vary across the mountain range by cloud cover, tree cover, terrain, and aspect. If you are pushing loose snow avalanches and they feel damp or dry, manage the problem through good slough management skills and skiing or riding one at at time. Recognize that as you descend the slope, these avalanches could move into wetter snow and transition to wet snow avalanches.
At low elevation, there is not enough snow to create D2 avalanches and danger is low.