Observation Date
12/7/2019
Observer Name
Gagne/Duvernay/Finco/Luther
Region
Salt Lake » Little Cottonwood Canyon » Alta Periphery
Location Name or Route
Upper LCC Perimeter
Comments
Went out to look at the snow surface ahead of the next storm expected on Sunday. In addition to the continued assessment of the persistent weak layer, wanted to answer a few questions:
1. Is the weak snow at the surface (surface hoar and near-surface facets) preserved or did the winds break it down?
For the most part, the winds destroyed the old weak snow at the surface, but I did find wind-sheltered pockets where weak snow has been preserved. But warm temperatures have helped break it down somewhat. From what I saw today I am not concerned about the Sunday storm snow falling on a weak, pre-existing snow surface.
2. Are there any sensitive wind slabs that have formed on top of the weak snow at the surface?
The southerly winds were sustained, but I was only finding pockets of fresh wind slabs, generally on northerly aspects. These slabs were up to 20 cms (8") thick and pencil-hard, but were not sensitive to stability tests (i.e. ski cuts). However, they are sitting on top of weaker snow, so I think it is possible there are some pockets of recent wind slabs that may be reactive to a trigger. Given the slabs were so stout, they also may allow someone to get well-out onto a slope before failing.
Video of snowpack discussion.
Video
Video showing full propagation with ECT. (ECTP21 failing down 90 cms on faceted snow.)
Video
Today's Observed Danger Rating
Considerable
Tomorrows Estimated Danger Rating
Considerable