Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Likely
- Taille
- 3
Other than a shallow avalanche or two, the snowpack has been rather well-behaved the past few days. Sure we've got plenty of weak layers, and we've got a bed surface, and no shortage of triggers, but we've been missing a key ingredient... a slab! And that all changed early this morning as strong winds are beginning to change the landscape. In fact, I'd expect to see a fresh batch of cohesive slabs already forming, especially along the leeward side of upper elevation ridges.
And remember- our Persistent Weak Layer, buried in the mid portion of the snowpack is in its teenage years and it doesn't take much effort to get it riled up. Yesterday, pro observer JG reported big booming whoomphing sounds and sudden collapses of the snowpack ... eerie indicators of a weak, rotten snowpack with a dense layer of snow on top. And that was before the wind started blowing! Here's where it gets tricky... the surface snow may feel good to go, but we need to think about not only the snow we're riding in, but also the snow we're riding on. And here's where it gets dangerous- any slide triggered will break several feet deep, and a couple hundred feet wide, failing on one of the many persistent weak layers of faceted snow in the snowpack (see JG's beautiful pit profile and comments below).
JG has decades of Uinta snow and avalanche knowledge and says this about our snowpack structure- " I have a low tolerance for risk based on our snowpack setup so I'm going to continue to avoid terrain 30° and steeper. "
Video describing how you can trigger avalanches from below.