Loose Wet
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 3
Wet Slab Avalanches: You should consider changing your plans if you had big mountain objectives in mind.
On slopes facing the north half of the compass it is possible people will trigger dangerous (wet) slab avalanches failing on a sugary, buried persistent weak layer, which is now pretty moist in most places. Unstable snow exists on slopes plagued by this buried persistent weak layer. The warmth softened existing slabs and crust layers, and increased creep and glide rates, which caused natural wet slab avalanches to become possible and triggered avalanches likely in steep terrain.
This large natural wet slab avalanche in the "Picture Window" area of Pine Canyon appears to have occurred on Sunday morning, since we did not see it with the glass on Saturday afternoon.
In most areas temperatures stayed well above freezing again overnight, and wet loose avalanches remain likely in the backcountry today. A bit of rain may soak the already saturated snow at lower elevations and mountain temperatures will rise into the mid forties during the day. When the snow surface becomes damp or unsupportable, it's time to head home. Watch for signs of heat-related instability like rollerballs, pinwheels, or sluffs of saturated surface snow. Wet slushy snow is generally unstable on steep slopes.