Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–1.5
How much wind slab you find at upper elevations on Monday will depend on two things: wind speeds where you are in the mountains and the amount of fresh snow on the ground. The melt-freeze crust buried in early February is a great marker to identify the amount of new snow that fell since last week.
At mid-elevations, there is maybe an inch or two and it's probably just not enough for significant wind slab development. 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.
Active wind transport should be easy to identify when winds are stronger in the morning. If winds are light, look for the usual scoured snow surfaces that show where the snow was stripped, and fat 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.
(2/4/2024)
Use differences in snow accumulation and texture to figure out where wind slabs might lurk.