Avalanche Forecast

Issued: Feb 14th, 2018 4:28PM

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

Avalanche Canada jlammers, Avalanche Canada

Storm slabs, persistent slabs and weak cornices make for a complex snowpack. I'd continue to choose conservative terrain and limit my exposure to overhead hazards.

Summary

Confidence

Moderate - Due to the number of field observations

Weather Forecast

Thursday: Mainly clear skies / Moderate to strong northwest winds / Alpine temperature of -18Friday: Overcast skies with light flurries / Moderate to strong westerly winds / Alpine temperature of -12Saturday: 3-8cm of new snow / Light and variable winds / Alpine temperature of -14

Avalanche Summary

We have received no new reports of avalanche activity, although that may speak more to a lack of observations rather than actual conditions. I suspect there was a round of storm slab avalanche activity in response to Tuesday night's storm. A very large, widespread natural avalanche cycle up to size 4 was observed last week. Slopes of all aspects and elevations ran full path and reached valley floor. In some cases, mature timber was destroyed. Many of these failed on persistent weak layers mentioned in the snowpack discussion. Although natural avalanche activity on these layers has tapered-off, human triggering of very large avalanches remains a very real possibility.

Snowpack Summary

By Wednesday morning up to 25cm of new snow had fallen. Wind data has been sparse, although I suspect strong winds shifted these accumulations into deeper, reactive slabs in wind-exposed terrain. These accumulations overlie a mix of older wind slabs in exposed higher elevation terrain, a sun crust on steep solar aspects and surface hoar on sheltered slopes.Below the snow surface, several persistent weak layers make up a troublesome snowpack. In the top 1-1.5 m of the snowpack, two surface hoar layers buried in January can be found. Expect to find at least one of these layers on all aspects and elevations.Deeper in the snowpack (120-200 cm deep) is a facet/crust/surface hoar layer from December, most prevalent at and below treeline.Near the base of the snowpack is a crust/facet combo, most likely to be triggered from thin spots in the alpine.All of these layers have produced large avalanches recently. The wide distribution and ongoing reactivity of these layers suggests that avoidance through choosing simple terrain is the best strategy.

Problems

Persistent Slabs

An icon showing Persistent Slabs
Several troublesome layers exist in the snowpack and may be reactive to large triggers such as a cornice or storm slab release. Human triggering may also be possible in shallow or thin, rocky areas.
Avoid steep convexities or areas with a thin or variable snowpack.Minimize exposure to overhead avalanche terrain, large avalanches may reach run out zones.Pay attention to overhead hazards like cornices which could easily trigger persistent slabs.

Aspects: All aspects.

Elevations: All elevations.

Likelihood

Possible

Expected Size

2 - 4

Storm Slabs

An icon showing Storm Slabs
New storm slabs may be especially reactive in wind-exposed terrain, and may be slow to gain strength due to a mix of underlying weak surfaces. Watch for new wind slab development and reverse loading due to forecast strong northwest winds on Thursday.
Stay off recent wind loaded areas until the slope has had a chance to stabilize.If triggered the storm slabs may step down to deeper layers resulting in large avalanches.The new snow may require several days to settle and stabilize.

Aspects: All aspects.

Elevations: All elevations.

Likelihood

Possible - Likely

Expected Size

1 - 2

Valid until: Feb 15th, 2018 2:00PM

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