Avalanche Forecast

Issued: Jan 28th, 2018 4:24PM

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

Avalanche Canada mgrist, Avalanche Canada

Warm storm coming! Avoid all avalanche terrain during periods of heavy snowfall, including exposure to overhead hazard.

Summary

Confidence

Moderate - Intensity of incoming weather systems is uncertain

Weather Forecast

Monday: 15 cm snow Sunday overnight into Monday. 15-25 cm additional snow during the day. Moderate to strong south-westerly winds. Alpine temperature warming in the afternoon to near -2. Freezing level rising to 1200m in the afternoon. Tuesday: 5-15 cm snow. Moderate south-easterly winds. Alpine temperature near -5. Wednesday: Isolated flurries (up to 5cm possible). Moderate southerly winds. Alpine temperature near -5.More information can be found in the Mountain Weather Forecast.

Avalanche Summary

On Saturday a human-triggered Size 2.5 avalanche was reported near 2300m on a south west aspect in Glacier National Park. See the MIN report for incident details. Locally heavy snowfall in the Monashees on Saturday produced a widespread natural avalanche cycle in the afternoon. A widespread natural avalanche cycle is expected with Monday's storm, with the potential for some surprisingly large avalanches given how many persistent weak layers exist in the snowpack.

Snowpack Summary

The current snowpack is complex, with three active weak layers that we are monitoring. The recent storm snow fell with strong south winds, producing wind slabs in lee features at treeline and alpine elevations and in open areas below treeline.1) 60-90 cm of storm snow sits on a crust and/or surface hoar layer from mid-January. The crust is reportedly widespread, with the possible exception of high elevation north aspects. The mid-January surface hoar is 5 to 20 mm in size and was reported at treeline elevations and possibly higher. 2) Deeper in the snowpack, the early-January persistent weak layer is 90 to 120 cm below the surface. It is composed of surface hoar on sheltered slopes as well as sun crust on steep solar aspects and is found at all elevation bands. Snowpack tests show sudden fracture characters and signs of instability such as whumpfs, cracking and avalanches. 3) Another weak layer buried mid-December consisting of a facet/surface hoar/crust combination is buried 100 to 150 cm deep. It is most problematic at and below tree line.

Problems

Storm Slabs

An icon showing Storm Slabs
Heavy snowfall and warming temperatures are a recipe for widespread avalanches. A storm slab could step down to a deeper weak layer, creating a surprisingly large avalanche.
If triggered storm/wind slabs may step down to deeper layers and result in very large avalanches.Avoid all avalanche terrain during periods of heavy loading from new snow, wind, or rain.

Aspects: All aspects.

Elevations: All elevations.

Likelihood

Likely - Very Likely

Expected Size

1 - 3

Persistent Slabs

An icon showing Persistent Slabs
Several weak layers are buried in the snowpack, creating very large avalanches when triggered.
Avoid open slopes and convex rolls where buried surface hoar may be preserved.Avoid steep convexities or areas with a thin or variable snowpack.Make conservative terrain choices.

Aspects: All aspects.

Elevations: All elevations.

Likelihood

Possible - Likely

Expected Size

2 - 4

Valid until: Jan 29th, 2018 2:00PM

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