Avalanche Forecast

Issued: Jan 30th, 2018 4:56PM

The alpine rating is considerable, the treeline rating is considerable, and the below treeline rating is considerable. Known problems include Storm Slabs and Persistent Slabs.

Avalanche Canada mgrist, Avalanche Canada

Conditions remain primed for human-triggered avalanches. Give the snowpack time to settle before pushing into more aggressive terrain: Simple terrain is recommended for now.

Summary

Confidence

Low - Due to the number of field observations

Weather Forecast

Wednesday: Cloudy with isolated flurries. Light westerly winds. Alpine temperature near -9.Thursday: Scattered flurries (5-10cm possible). Light to moderate south-westerly winds. Alpine temperature near -8. Friday: Snow (10-20 cm). Moderate southerly winds. Alpine temperature -8. More information can be found in the Mountain Weather Forecast.

Avalanche Summary

On Tuesday we received preliminary reports of an avalanche involvement in the north Columbia region near Clemina creek. The avalanche ran on a north facing aspect near 1900m. A natural storm slab avalanche cycle occurred on Monday with heavy snow and temperatures up to +2 Celsius in some tree line locations. See this MIN report for a good example of the avalanche activity. Conditions remain primed for human triggered avalanches, with the potential for some surprisingly large avalanches given how many persistent weak layers exist in the snowpack.

Snowpack Summary

25-40 cm of storm snow fell from Sunday through to Tuesday and temperatures spiked to -2 at tree line in the south of the region (and +2 near Barkerville) on Monday afternoon. The new snow sits on a complex snowpack and there are three active weak layers we are monitoring:1) Down about 40-80 cm is a crust and/or surface hoar layer buried mid-January. The surface hoar is up to 10 mm in size, found at all elevation bands and very reactive on north east aspects between 1900-2600m.2) Deeper in the snowpack, the early-January persistent weak layer is found 50 to 100 cm below the surface. 3) Another weak layer buried mid-December consisting of a facet/surface hoar/crust combination is buried 100 to 150 cm deep. It has been most problematic at and below tree line.See here for a good summary of snowpack test results.

Problems

Storm Slabs

An icon showing Storm Slabs
Warming temperatures put heavier snow on top of lighter dry snow - a recipe for an unstable snowpack. A storm slab could step down to a deeper weak layer, creating a surprisingly large avalanche.
The new snow will require several days to settle and stabilize.Avoid exposure to overhead avalanche terrain, large avalanches may reach the end of run out zones.Be wary of slopes that did not previously avalanche.

Aspects: All aspects.

Elevations: All elevations.

Likelihood

Likely

Expected Size

1 - 2.5

Persistent Slabs

An icon showing Persistent Slabs
Several weak layers are buried in the snowpack, creating very large avalanches when triggered.
Avoid steep convexities or areas with a thin or variable snowpack.Make conservative terrain choices, remembering that avalanches may be surprisingly large.

Aspects: All aspects.

Elevations: All elevations.

Likelihood

Possible - Likely

Expected Size

1.5 - 4

Valid until: Jan 31st, 2018 2:00PM