Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–1.5
Upper elevations vary in the amount of new snow above the crust. Some places have up to 6” while others are already quite scoured down and have nothing left to offer up for fresh slabs. You'll easily be able to identify the new snow depth as the amount above the early February crust. Any avalanches may slide far and easily on the crust surface.
Active wind transport is an easy identifier for wind loading, but winds are forecasted to be light, so new slabs probably aren't forming. Look for the scoured snow surfaces that show where the snow was stripped, and drifts where it ended up. Stomping on features like tiny cornices and test slopes will be the best way to see if there is any reactivity in the fresh slabs.
Example photo: There's a very small chance you could trigger very small wind slabs on leeward sides of features at upper elevations, like this one, on Tuesday.