Summary/history of the problem-
- Snow fell in October & early November
- Dry weather from early November to early December weakened and faceted that snow which became the "persistent weak layer"
- That snow melted away on south facing slopes
- Heavy snowfall in December buried that weak layer and caused avalanches on it
Current situation-
All the ingredients for an avalanche exists with a weak layer near the ground and a very thick, deep, and hard slab of snow on top of it (3-5' deep). What is lacking is the weight and stress from recent snowfall. The last snowfall was 6 days ago, and the last reported avalanches was 8 days ago.
The good news-
The weak layer has gained A LOT of strength, and it is hard to impact the weak layer which is buried so deeply. Triggering a slide on slopes with a deep, uniform snowpack is unlikely.
What to watch out for-
The weak layer is the weakest and easiest to impact in upper elevation, rocky, alpine terrain above treeline. These are places where snow depths are much more variable and the weak layer remains weak in isolated pockets. There is a possibility of triggering a slide in those locations.
A regular observer in
upper Weber Canyon found similar conditions as well with a deep and strong snowpack that is giving us more and more confidence to start stepping out into avalanche terrain.
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ALSO of note - As Craig found yesterday
in upper Weber Canyon, slopes that previously avalanched sometimes become future problems (repeaters) but most of them slid during December storms and immediately refilled with snow. For that reason, they have a slightly shallower snowpack, but the weak layer has become stronger on those slopes just like on ones that didn't slide.