Wind Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Likely
- Taille
- 1–2
Thursday will be the final day of a 3-day storm cycle. Although snowfall peaks Wednesday afternoon through the night, wind speeds likely peak on Thursday. We're expecting significant wind redistribution throughout the day on Thursday, maintaining slab reactivity as slabs also increase in size. Focus on the degree of fresh and recent snow transport rather than decreasing snowfall rates. If you see large plumes of snow coming off ridgelines, slabs on the slopes below will be fresh and reactive. Even if wind loading dies down, drifts will be recent and need more time to settle out. Look for fresh, sharp cornices overlooking suspect slopes. Slabs may form in the lee of ridges or well down on the slope, such as on poorly supported rolls in the terrain. In some cases, extreme wind gusts could scour start zones and deposit most of the snow down in canyon bottoms. Gauge the depth of the snow above the 3/13 crust and steer around any steep slopes where you suspect deeper deposits. Slabs could fail on density interfaces above the crust or pull out down to the crust. The crust has a slick and more concerning bed surface in upper elevation terrain, where we are also expecting thicker drifts, combining to form larger and more widely propagating avalanches. Give yourself an extra margin for safety, limiting your exposure to activly loading slopes above you, which could produce isolated natural avalanches.
At lower elevations, we're looking at shallower amounts of new snow above the crust. Winds may form isolated slabs near more exposed ridgelines. Steer around lens-shaped pillow-like drifts on steep slopes.
Example: Heavy drifitng along Pea Gravel Ridge
Photo: Joe Dellaporta