Wind Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Likely
- Tamaño
- 1–2
New windslabs have formed in the immediate lees of features and are up to 40 cm deep. This is different from the windslabs described in previous days.
15-35 cm of recent light snow is not bonding well to the underlying snow. Choose lower angle terrain for riding and carefully select climbs to manage the new problems.
New windslabs have formed in the immediate lees of features and are up to 40 cm deep. This is different from the windslabs described in previous days.
This problem represents both the Dec. 2nd crust/ facet layer (treeline and below) and the late December facet layer. Lots of variation in the sensitivity ranging from reactive sudden collapse to no results depending on location, aspect and elevation.
There is a touchy storm snow interface, down 15-35 cm, on surface hoar/crust/facets buried on Jan 30. Steep rolls with >20 cm of snow are most reactive, if they have not already slid.
As the Arctic air slides into the region for a short visit, temperatures will noticeably drop in the afternoon as the winds shift to light from the North. The coldest day will be Wednesday where morning temps will be in the -25 range with sunny skies and then warm through the day and into Thursday.
15-35 cm in the last 24 hrs has created fresh windslabs and surface instabilities that are bonding poorly to the underlying surface of surface hoar/crusts/facets. Expect easy triggering of these soft slabs. It's unlikely to wake up the deep facets, but they continue to lurk 100-180 cm deep & could be triggered by cornice failures should they occur.
New wind slabs were ski & explosive triggered in the immediate lees by the ski hill snow safety teams. In Yoho, numerous storm slabs observed/triggered in steep terrain. Over the past week there have been a few avalanche to sizes 3 on the persistent weak layer. All were triggered by large loads (cornice).