The near-surface facets (NSF) that formed during the long stent of high pressure are now buried underneath roughly 18 to 32 inches of new snow in the upper Cottonwoods. Resting on top of these weak crystals lies a 4 finger slab (out of the wind zone) that is enough weight to get results in our snowpits. Natural activity on this layer during the storm was observed in our travels today. In the wind zone, on leeward slopes and terrain features, I would expect these avalanches to be more connected and more destructive. We dug on a west-facing slope to confirm our suspicion and verify the forecast of the PWL and the results can be seen in the video below.

Winds were coming from all over the compass during the storm, and I suspect these freshly formed wind slabs to still be reactive to the weight of a skier or boarder. The issue is where the wind has blown snow on top of the slopes where the Persistent weak layer exists. This problem will not settle out quickly. The wind-driven snow has added a more stiff slab and is stressing this weak layer even further.