Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Unlikely
- Dimensione
- 1.5–2
What is it? Although it's not likely, the most plausible way to get in trouble is in wind-affected alpine terrain, which Ethan explains in the video to the right/above. There is an outside chance of triggering buried surface hoar down 1-1.5 feet, but the evidence is growing harder to find. See the Forecast Discussion below for more information on the Wood River Valley conditions.
Where is it? You're most likely to find the problem where the wind has loaded slopes or stiffened the snow surface. The surface hoar is most problematic in somewhat protected, middle-elevation terrain that faces NW-N-NE. These layers are most likely triggered on slopes steeper than about 35 degrees.
How can you recognize it? Wind-loaded slopes have harder surfaces and a distinct appearance (video to right/above). You may or may not experience snowpack collapsing and/or cracking while traveling. These red flags are obvious signs of instability. The surface hoar layer is subtle and may not "jump out at you" when searching for it in a snowpit (see photo here).
How can you manage it? You can reduce your risk by avoiding very steep (greater than about 35 degrees), shady slopes (facing W-N-E) with hard or stiff wind-blown snow at the surface—especially those with ugly consequences if you are caught in an avalanche. Persistent slab avalanches may break wider than expected or higher on the slope above you.