Wind and storm snow have formed cohesive slabs above the recently buried crust/ surface hoar layer at upper elevations. It may also be possible to trigger a buried weak layer from thin snowpack areas.
Avalanche Problem 1: Wind Slabs




- Be careful with wind loaded areas, especially near ridge crests and roll-overs.
- If triggered the wind slabs may step down to deeper layers resulting in large avalanches.
Avalanche Problem 2: Persistent Slabs




Weak layers buried in the snowpack have produced recent avalanches with very light triggers particularly on unsupported features at lower elevations.
- Watch for signs of instability such as whumpfing, or cracking at lower elevations.
- Avoid shallow or thick to thin snowpack areas where triggering a deeper layer is more likely.
Avalanche Summary
Friday there was a report of a helicopter remotely triggering a Size 2.5 wind slab from above the slope on a west aspect at 1500 m north of Kispiox.
Thursday there was a report of skiers, north of Kispiox, remotely triggering a Size 2-2.5 avalanche from a safe location on a ridge that released on the adjacent slope on a northwest aspect at 1650 m. A weak layer buried late-December was the suspected failure plane.
Wednesday there was a report of a skier-triggered Size 1 wind slab avalanche on a northwesterly aspect at 1650 m in the northern part of the region, east of Ningunsaw.
Tuesday there were reports of easily-triggered wind slabs 30-40 cm deep releasing to Size 1 in wind-loaded areas near ridge crests in the alpine in the southern part of the region.
Reports from late last week showed a notable increase in persistent slab activity at lower elevations in the Howson Range. In this area, three Size 2 releases failed on steeper terrain with remote triggers on the mid-December weak layer, found 50 cm below the surface.
Snowpack Summary
Recent light snowfalls have gradually brought 20-60 cm of new snow across the region. This new snow has buried the mid-January interface which features a crust that exists well into the alpine and isolated pockets of surface hoar in sheltered areas at lower alpine and treeline elevations.
Below the mid-January interface, deeper weak layers in the snowpack include two separate crust and surface hoar layers that were buried late-December and mid-December and now lie 50-80 cm below the surface. In the past week these deeper layers have produced hard but sudden results in recent snowpack tests as well as recent large avalanches triggered from a distance.
Weather Forecast
TONIGHT: Increasing cloud. Ridge wind light, southeast. Temperature -15. Freezing level valley bottom.
SUNDAY: Cloudy, flurries. Accumulation 2-5 cm. Ridge wind strong, southeast. Temperature -12. Freezing level valley bottom. Alpine Inversion.
MONDAY: Cloudy, flurries. Accumulation 5-10 cm. Ridge wind strong, southwest. Temperature -8. Freezing level 200 m.
TUESDAY: Cloudy, flurries. Accumulation 2-5 cm. Ridge wind moderate, southwest. Temperature -10. Freezing level valley bottom.
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Wind slabs can be found on leeward aspects in the alpine as well as wind-exposed areas at treeline. These slabs overly a thin crust/ surface hoar layer and have been reactive to light triggers especially in steep or convex terrain near ridge crests.