Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible - Likely
- Size
- 1–2.5
Storm snow is expected to remain reactive to human triggers. It sits over dense wind affected surfaces and is taking some time to gain strength and bond. Greater slab quality and propagation has been seen in wind affected terrain, while in sheltered areas storm snow is reacting as loose dry sluffing.
A layer of buried surface hoar may increase reactivity and produce larger avalanches than you expect - this is more likely to be found in sheltered and shaded terrain features. Reports suggest this is most prominent in the northern areas of the region.