Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
We're not quite sure how reactive recently formed wind and storm slabs will remain on their second day. Increasing temperatures could help 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, which could mean an improvement in stability, or possibly 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, and taking into account reactivity may change throughout the day.
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 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.
(2/21/2023)
Example photo: you could still trigger small or large slab avalanches on Wednesday. These are more likely to happen in wind loaded areas, but may happen in non wind loaded areas as well. Baker NRA.