Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2
Persistent slab avalanches can catch even the most experienced backcountry travelers by surprise. They can break widely around terrain features and be triggered from lower angle slopes. There is lots of variability in the snowpack, and we don't have a good handle on it, especially while we are in the midst of a storm cycle such as this one. In any case, numerous reports of loud whumphing tell us that we may be reaching a tipping point, and the triggering of these slides may be fairly easy to do. This instability dominates the way we think about, and plan to travel in the backcountry because all slopes steeper than 30 degrees are suspect. Look for a thin layer of weak snow above or below a crust roughly 14"-24" down from the surface. There may be a layer of buried surface hoar a few inches above this crust as well. Whumphing and collapsing of large sections of snow direct signs that the snowpack is unstable.
On Thursday an observer reported whumphing on Delancey Ridge, and snowpack tests indicated failure on weak snow below the crust at low elevations (South at 3,900ft). On Wednesday multiple observers experienced whumfping collapses, signs that a persistent slab problem may be primed to wake up. Dig down to look for weak sugary snow above a firm crust at all elevation bands. Stiff, wind drifted slabs may be found at upper elevations. Places where firm, drifted snow covers steep slopes will be especially important to avoid on Friday, as any slide triggered in wind stiffened snow has the potential to be a much larger avalanche.
Widely propagating crowns such as this are characteristics of persistent slab avalanches.