Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 2
There is a fair bit of capital U Uncertainty here in regards to the snowpack. The warmth (over the past week(s) and rain has dampened the snow from the top down and the bottom up and we have an 'isothermal' snowpack in many areas. The lingering problem, however, is that the poor structure still exists and I think it's still possible for someone to trigger an avalanche that fails on one of two layers of faceted snow (PWLs). That is, if they can collapse the superficial crusts. Mark White found this poor and unstable structure along the Park City ridgeline yesterday (video below) on northwesterly facing terrain at 9500'. Time will tell how this whiplash in temperatures will affect the structure in the coming days. What I will say is that the risk matrix for getting on steep polar terrain today registers as moderate risk but with very low reward.
And...just to add more complexity to the overall picture: rain crusts are notorious for both connecting slopes together AND fostering the development of weak, faceted grains. We'll be watching with interest.