I just don't trust this structure. Our Dry January Layer (DJL) of faceted snow is now buried one to three feet deep and is the weak layer for four avalanche fatalities and more than 60 reported avalanches. The slab on top of the DJL has gained strength, and signs of instability - such as collapsing - are no longer common. But an avalanche failing on this layer will be up to three feet deep, and possibly hundreds of feet wide. Spatial variability, rain on snow, and warm temperatures complicate things:
- At upper elevations, you are more likely to trigger an avalanche where the snowpack is thinner. In my field work on Sunday along the Park City Ridgeline, I observed spatial variability where some slopes had a thick, strong slab on top of the DJL, and others where the slab was thinner and I was able to get full propagation with extended column tests. A similar structure exists in the Provo mountains.
- At mid elevations, warm temperatures and rain on snow has further weakened the DJL, and wet slabs failing on moist, weak grains at our DJL are possible, such as a recent avalanche on Brighton Hill in the photo below.
I will continue to avoid steep, northerly-facing slopes, and fortunately, recent dense snow and warm temperatures have smoothed out the snow surface, providing decent travel and riding conditions on slopes less than 30° in steepness.
