Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
What is it? Within 48 hours, skiers have triggered five different avalanches in the Wood River Valley (see Media gallery below). If that information isn't alarming on its own, a large cycle of natural avalanches produced widespread activity across this area. Today, you can find the same sensitive 1-3 foot thick slabs in many areas with the recent wind-affected snow.
Where is it? These slabs will be the largest and thickest at upper elevations, but you'll also find wind slabs in exposed lower and middle elevation terrain. The foothills around town saw wind-affect early in the storm and can be subtle or hidden by newer snow. Be on the lookout for wind slabs from the valley bottom to the mountain tops, and expect them to be easy to trigger. Even the slightest change in slab stiffness can have an effect on the weak snow below.
How can you recognize it? Cracks shooting out from your skis or sled and collapsing clearly indicate instability. Look for ripples in the snow, dunes capping ridgelines, and drifts along the sides of gulleys or chutes. Wind-deposited snow will be stiffer and keep your skis or snowmobile on or closer to the surface. Some of these slabs might be masked by recent snow and be more hidden.
How can you manage it? Most wind slabs are building on top of persistent weak layers in the snowpack (read Problem #2 below). Because of this, the wind slabs you encounter today may behave more like persistent slabs than "simple" wind slabs. Fresh slabs will be reactive to your weight and may produce avalanches that break wider and deeper than you might expect. Triggering these avalanches remotely (from a distance above, below, or to the sides of steeper slopes) is a real possibility.
(3/5/23) These large avalanches failed naturally in wind-affected areas on a N-E facing slope at 7000-8400'.