Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Use caution on leeward slopes over 35 degrees where westerly wind deposited storm snow on the 10-11th. Along with typical drifting below ridges, you may find wind-stiffened snow in unusual locations and lower on slopes than usual. With the previous strong winds, many surfaces are stiff and wind-textured. It's important to distinguish where the stiff surfaces transition, becoming deep enough for wind slabs. You can use your probe or pole to feel for how thick these slabs are, and consider steering around steep slopes where it's more than just a few inches thick. While the likelihood of triggering a wind slab is decreasing with mild weather, this weak interface is lingering longer than a typical windslab. You can use simple tests like hand shears, test slopes, and tilt tests to evaluate the bond. Recent avalanches and cracks shooting through the snow are "red flag" indicators of the danger.
There's a chance that you could still trigger isolated avalanches in very steep, wind-sheltered terrain. 7-9" of recent snow rests on a variety of thin, weak layers, including stellars, facets, or surface hoar over a crust. The crust is most prominent on steep southerly aspects and below 5,100ft. There is a lot of variability in the weak layer and crusts below the storm snow and wind slabs, complicating these problems. So, give yourself some additional margins of safety to account for this uncertainty.
(1/11/2025) Crown of intentionally triggered windslab, NW ridge Tye Peak. Photo: Ryan Minton