Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Likely
- Taille
- 1.5–3
It is possible for skiers and riders to trigger large hard slab avalanches failing on weak snow that formed during December. These slabs are 2-4 feet deep above 7,500’ and 1-2 feet deep below that. Most aspects remain suspect because of the widespread nature of the January 4th persistent weak layer. Triggering an avalanche is most likely between 7,500’ and 9,000’ due to a thinner slab and well preserved weak layer, but should not be ruled out on steep slopes at the higher elevations. These slabs will become more sensitive to human triggers as temperatures rise today. A remotely triggered avalanche that occurred two days ago indicates that triggering a slide from a distance is still possible in the middle elevations. Steep, rocky, and unsupported terrain features are most likely to produce an avalanche at the moment. However, given the well connected nature of the weak layer, it is possible for avalanches to propagate long distances across or up slopes. Because of this, careful evaluation of the terrain that you plan to ride, as well as the surrounding slopes is important. Avoid crossing underneath steep slopes, especially this afternoon, and give consequential terrain features (gullies/cliffs) a wide margin.
Although unlikely, there is a chance that an avalanche failing on the January 4th interface could step down to weak snow at the base of the snowpack resulting in a very large avalanche.
Additional Discussion
For those traveling to the highest portions of the forecast zone, beware of shallow (less than 6”) wind slabs that may have formed from the light snow we have received over the past week. These slides will be isolated to very steep, wind loaded features in the upper elevations such as couloirs. A small slide that knocks you off your feet in serious terrain can have severe consequences.
A remotely triggered avalanche that occurred on 1/27 outside the JHMR boundary. Note the convex, rocky, and wind affected nature of the terrain.