Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–1.5
Increasing wind speeds are nearly guaranteed. The extent of wind slab formation will depend on how much soft and dry snow is available for transport. This is most likely at upper elevations, where more snow accumulated in the last few days, and temperatures stayed cooler. If you find dry snow and strong wind at mid elevations, then the danger is a bit higher there as well. Fresh slabs forming over a slick crust can be especially reactive.
Actively blowing or drifting snow will show you which slopes are loading up. Track the depth of wind drifted snow as you gain elevation or change aspects. This should be easy to do with a crust below the new snow in most places. Simple tests like hand pits and stomping on wind drifted features can help you gauge stability.
Blowing snow makes it pretty easy to figure out which slopes are getting loaded.
Photo: Joe Dellaporta