Wet Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Triggering wet slab avalanches remains possible on steep slopes. These conditions may be most widespread where the snowpack has gradually warmed, such as shady, mid-elevation slopes and upper elevation slopes facing southeast and west. In this terrain, meltwater may still be percolating into weak layers buried around crusts that formed in December. The likelihood of natural wet snow avalanches is diminishing. However, careful route selection continues to be essential because of the potential size and consequences of slides like these.
Avoid traveling on or below steep start zones, particularly those under rock bands and receiving direct sun. Exit avalanche terrain early, particularly where your route will take you through the runouts of steep start zones.
Keep in mind that wet snow avalanche hazards can be unpredictable, particularly when inversions are present like they are this morning. Slopes with a refrozen snow surface are unlikely to avalanche, though you can't tell if these crusts exist at higher elevations. And a wet snow surface tends to give few clues to how meltwater is percolating and whether slabs are becoming unstable.
(1/31/2024) Peter's Ridge, Northern Swan. Avoid traveling in or under terrain like this today.