Fresh wind slabs are forming at higher elevations, and have the potential to step down to a lingering persistent weak layer. Watch for signs of instability and choose conservative routes.
Problèmes avalancheux
Wind Slabs
N
NE
E
SE
S
SW
W
NW
Alpin
Limite forestière
Sous la limite forestière
Probabilité
Likely
Taille
1–2
Wind slabs can be expected on all aspects as winds will shift from the southwest to the northeast.
Persistent Slabs
N
NE
E
SE
S
SW
W
NW
Alpin
Limite forestière
Sous la limite forestière
Probabilité
Possible
Taille
2–3
40-80 cm of snow sits above a weak layer of facets from mid-December and continues to be reactive in parts of the region that have thinner snowpacks.
Weather Forecast
SUNDAY: Morning flurries easing off in the afternoon, moderate northeast winds, alpine temperatures around -18.MONDAY: Mix of sun and cloud, light east winds, alpine temperatures around -22.TUESDAY: Sunny with cloudy periods, light east winds, alpine temperatures around -18.
Confidence
Moderate - Wind speed and direction is uncertain
Avalanche Summary
On Friday, there were numerous reports of size 2 avalanches including natural and skier-triggered loose dry avalanches and explosive-triggered wind slabs. There were also isolated reports of size 2 storm slabs on Saturday, including one that stepped down to glacial ice on a steep south-facing slope. Expect touchy wind slabs to develop as moderate winds redistribute loose snow in exposed terrain.Also, a notable MIN report from Friday shows what seems to be a size 2 persistent slab that was triggered by a ski cut in a cutblock west of Kimberly (see MIN report from Mallandaine Pass). This is a reminder that although avalanche activity on persistent facet layers has been intermittent, the problem will likely linger for some time in shallow snowpack areas.
Snowpack Summary
The region received a total of 40-60 cm of low density snow over the past week. Recent winds have come from a variety of directions and have loaded leeward and cross loaded features in exposed terrain. An interface that formed during the early December cold snap can be found buried 40-80 cm deep. The interface may consist of stiff wind-affected snow, faceted (sugary) crystals, or surface hoar crystals. The overlying slab appears to have a poor bond to the interface in some areas, such as wind-affected terrain in the Dogtooth range and shallow snowpack areas like the southern Purcells. The thick mid-November crust and facet layer is now buried 70-150 cm deep and appears to be dormant.