Strong winds have created touchy slabs at higher elevations. Human triggered avalanches remain likely at all elevation bands. Choose conservative terrain and be aware of overhead hazard, especially on sunny aspects.
Avalanche Problem 1: Wind Slabs




- Avoid lee and cross-loaded terrain near ridge crests or convex rolls.
- Watch for whumpfing, hollow sounds, shooting cracks or recent avalanches.
- Be aware of the potential for wide propagations.
Avalanche Problem 2: Persistent Slabs




Weak layers buried 100-150 cm below the surface have been reactive in recent snowpack tests and have also produced a few large avalanches recently. These layers may remain sensitive to human triggering in shallow snowpack areas.
- Avoid lingering in runout zones, avalanches triggered up high may run long distances.
- Avoid shallow or thick to thin snowpack areas where triggering a deeper layer is more likely.
Avalanche Summary
On Saturday we received several reports of natural avalanches to size 3 (particularly on northeast facing slopes at higher elevations) as the winds picked up and slab avalanches ran surprisingly far. See this MIN post for more information. See here for a stunning photo of a large avalanche.
Also on Saturday, explosives control produced size 2.5 avalanches in below tree line terrain north of Smithers.
Numerous natural storm slab avalanches up to size 2 were reported to be running in steep terrain during the storm on Wednesday in the southern part of the region. See here for a good summary of avalanche activity near Smithers.
Snowpack Summary
Strong north west winds picked up on Saturday, redistributing last week's storm snow and creating fresh wind slabs at higher elevations. A strong inversion also set up with tree line temperatures near 0 degrees.
Wednesday's storm delivered between 15-50 cm of new snow, bringing totals to 40-100 cm over the past week. Areas near Smithers and farther south saw higher snowfall amounts than areas to the north.
A crust and/or weak feathery surface hoar layer buried in mid-January now lies about 100 cm below the surface. The crust exists well into the alpine and the surface hoar can be found in sheltered areas in the lower alpine and tree ine elevations. Recent snowpack tests produced hard, sudden results on weak, sugary snow crystals associated with this crust in the Smithers area, indicating that this is still a layer of concern to watch for.
Another two crust / surface hoar layers that were buried in December are now 100-150 cm below the surface. These layers produced sudden results in recent snowpack tests and have been the suspected weak layer in recent large remotely (from a distance) triggered avalanches.
Weather Forecast
Strong northerly winds and sun effect are the main weather factors on Sunday. Small snowfall amounts on Tuesday.
SUNDAY: Mostly sunny. Ridge wind moderate to strong from the north / east. Temperature -7. Freezing level valley bottom.
MONDAY: Increasing cloud in the afternoon. Ridge wind strong from the northwest. Temperature -6. Freezing level valley bottom with an above freezing layer between 1400m and 1900m.
TUESDAY: Snow (5-10cm). Ridge wind strong, southwest. Temperature near -4. Freezing level 400 m.
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Strong northerly winds produced reactive wind slabs in exposed areas at tree line and above. Expect these slabs to be reactive to human triggering and keep in mind that a release may also step-down to a deeper layer buried in the snowpack.