Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Recently formed wind and storm slabs may remain reactive on their second day, although we're uncertain how exactly they'll behave. Increasing temperatures could improve stability, or they could cause more "slabby", cohesive surface layers that could avalanche - maybe even without a human trigger. Expect a change in slab reactivity during the day, possibly leading to an improvement in stability, or maybe the other way around. Don't let the blue skies lull you into a false sense of security without having throughly investigated the new snow layers.
Use small test slopes and smaller features to test reactivity. Search for any "upside down" feeling snow underfoot or with your hand. If you're on foot, skis, or snowshoes "upside down snow" is not as pleasant for travel, with a firmer surface layer and softer, punchier snow beneath. If you notice this, avoid nearby slopes with these characteristics greater than 35°. In general, avoid large, steep, unsupported slopes while the snow continues to settle the day after the storm. Also, steer clear of slopes above terrain traps.
Snow may still slide whether it's been wind-affected or not, although smooth or textured, firmer wind slabs - usually near or around rocky outcroppings, on the side of steep rollovers, and in gullies- are suspect for remaining reactive longer than non-wind-loaded features.
Example photo: A small test slope with a small wind slab was reactive to a human trigger. Use small features like these on Wednesday to check for reactive pockets. Even if you don't see results as obvious as this, that doesn't mean that a large, convex, unsupported slope might not slide.
Photo: Kyle Wyatt