Recent snow and strong southerly winds have formed wind slabs on lee features at treeline and above. Use caution when transitioning into wind affected terrain.
Lingering wind slabs remain possible to human trigger in isolated areas. Wind slabs in motion may step-down to deeper weak layers resulting in large avalanches.
Triggering large avalanches on weaknesses in the lower snowpack remains a possibility. In some areas the concern is weak snow around crusts 60 to 90 cm deep, while in others it is weak snow near the bottom of the snowpack. Human triggering of these layers are most likely in steep, rocky slopes with a shallow or thin to thick snowpack.
FRIDAY NIGHT: Partly cloudy / Light, southwest ridgetop wind / alpine low temperature -11 / Freezing level valley bottom.
SATURDAY: Mix of sun and cloud / Moderate to strong, southwest ridgetop wind / alpine high temperature -8 / Freezing level valley bottom.
SUNDAY: Cloudy with isolated flurries; 0-3 cm. / Strong, southwest ridgetop wind / alpine high temperature -7 / Freezing level valley bottom.
MONDAY: Cloudy with flurries; 3-5 cm. / Moderate, southwest ridgetop wind / alpine high temperature -5 / Freezing level valley bottom.
Avalanche activity is beginning to slow down. However, previous to Thursday, there had been steady reports of natural wind slab avalanches in alpine terrain (size 1-2), and some smaller human-triggered wind slab avalanches in lee terrain (size 1). There are good photos of these avalanches in recent MIN reports (e.g. here, here, here, and here). While there have been no reports of persistent slab avalanches since Dec 22, there have been recent reports of large whumpfs in the Hudson Bay, Hankin, and Babines area, suggesting that buried weak layers are still possible to human trigger.
Strong wind is moving around 40-60 cm of snow that has fallen since New Year's Day. Reactive wind slabs can be found in exposed open terrain, while lower density snow can be found in sheltered terrain. In some parts of the region this snow could be sitting above a surface hoar layer and forming isolated persistent slabs on steep rolls in sheltered areas below treeline.
The lower snowpack has two crusts with potentially weak snow around them. Reports from the Smithers area suggest the upper crust is 60-90 cm below the surface and has shown signs of being possible to trigger from shallow areas. The other crust is near the bottom of the snowpack, and is most likely to trigger from steep, shallow, rocky slopes, with a thin to thick snowpack.
