Loose Wet
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
As the wet avalanche cycle continues, the avalanche size distribution changes. The larger, less predictable, and scarier type of wet loose slide should be your focus after several nights without a good refreeze. These avalanches occur in more isolated areas. You will primarily see them release naturally near and below cliffs on E-S-W aspects, but they start to entrain onto N aspects if the snow becomes heavy and wet. With 1-2 ft of snow above the 3/21 crust to potentially entrain, these avalanches could be large. Travel early and reduce your exposure to larger terrain features once the crusts break down.
Some aspects are further along in their spring transition and are trending toward homogeneity. In these areas, you may trigger the smaller and more predictable wet loose avalanches once the surface crust softens and the wet snow becomes deeper than your ankle. When you find wet, saturated snow, head to more shaded aspects or lower-angled slopes. These avalanches are most likely in areas receiving direct sunshine.
Example: A large natural avalanche from the Byrant Peak Couloir. This slide likely released as a spring shed from the looker's righthand cliffs. E, 5000'.
Photo: Dallas Glass