Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2.5
You could trigger 1-3 foot thick avalanches on buried weak layers (sugary facets or crust + facet combinations). The steady stream of snowfall and windblown snow has many slopes teetering on the edge, just waiting for a trigger.
The distribution, character, and sensitivity of the weak layers vary from slope to slope. Your best bet is to assume this problem exists and choose terrain accordingly. Conditions are most dangerous where wind slabs and drifts have formed a thicker, more cohesive slab. However, the snowfall from the past couple of weeks has become cohesive enough to act as a slab on most sheltered slopes.
You can reduce your risk by avoiding slopes steeper than 30 degrees—especially large avalanche paths and those with ugly consequences if you are caught in a slide. Persistent weak layers can fail unpredictably and break significantly wider, deeper, and higher on slopes than you might expect, producing much larger avalanches. You could remotely trigger avalanches from gentle terrain above, below, or to the sides of steep slopes. Avalanches could be triggered by the second, third, or fourth rider on a slope.
ADDITIONAL DISCUSSION: Small amounts of snow and light to moderate SW-S-SE wind over the past 36 hrs may have combined to build fresh, thin, sensitive wind slabs. Look for them near ridgelines and mid-slope terrain features like ribs and gullies. Small wind slabs can make effective triggers for the larger persistent slab avalanches described above.
(2/28/2023) NE face of Copper Mountain at 8,400'. This avalanche appeared to be remotely triggered by a skier from above. This crown in sheltered terrain (great skiing and riding conditions) is an excellent example of a slope that did not need wind loading to become unstable.