Wet Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
What and where is it: Wet slab avalanches are the primary concern during daylight hours as rain and warming temperatures affect the snowpack. While the snowpack is generally stable, isolated areas on northeast, east and southeast aspects still hold a buried weak layer (OBS1, OBS2) that could become more reactive as water percolates into the snowpack.
How can you recognize it: A wet snowpack is the obvious red flag. Rain on snow, rapidly increasing boot penetration, and heavy, saturated snow all indicate deteriorating stability. In addition to wet slabs, watch for loose wet avalanches in areas where unconsolidated snow lacks structure. This is most likely where deep, pooled graupel was observed yesterday, as these deposits can lose cohesion quickly once water is introduced. Determining where buried weak layers exist will be challenging or impossible during periods of heavy rain, so treat any steep slope with wet snow as suspect.
How can you manage it: Conservative decision-making will provide important margins of safety today. Avoid steep terrain where the snow is wet or becoming wet, and stay out from under avalanche paths as rain and warming intensify. Stick to lower-angle terrain and avoid gullies and other terrain traps where even a small slide can have serious consequences.