Avalanche Forecast

Issued: Feb 8th, 2018 5:14PM

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 cgarritty, Avalanche Canada

Deep and reactive new storm slabs have formed on an unstable snowpack capable of producing very large avalanches. A Special Avalanche Warning is in effect in this region. Copy this address to view details: http://bit.ly/2nSOUyX

Summary

Confidence

High -

Weather Forecast

Friday: A mix of sun and cloud with gradual clearing over the day. Light north winds. Alpine high temperatures to -12.Saturday: Mainly sunny with valley cloud due to an alpine temperature inversion. Light southwest winds. Alpine high temperatures to around -9, cooler at lower elevations.Sunday: Mainly sunny with valley cloud due to a lingering temperature inversion. Light southwest winds. Alpine high temperatures to -8, cooler at lower elevations.

Avalanche Summary

Wednesday's reports included observations of storm slabs releasing both naturally and with ski cutting from size 1-2. No new persistent slab releases were observed in the North Columbias.On Tuesday, numerous storm slabs were triggered naturally, by explosives, and skiers. They were small to large (size 1 to 2), on all aspects, with depths from 20 to 40 cm. Persistent slab avalanches were large (size 2 to 3), explosives-controlled, 100 to 200 cm deep, on all aspects, and generally releasing on the late-November crust.Monday's reports showed evidence of a natural avalanche cycle from Friday to Sunday, with widespread storm, wind, and persistent slab avalanche activity. The persistent slabs released on all aspects and on all of the layers discussed below. Crown fractures ranged from 100 to 400 cm deep.Expect dangerous snowpack conditions to persist on Friday as our snowpack adjusts to the new load. A stable weather pattern in the forecast suggests we may see a decrease in natural avalanches, but human triggering remains a big concern. Storm and wind slabs have the potential to step down to deeper weak layers, which could produce very large avalanches with high consequences.

Snowpack Summary

25-70 cm of new snow fell during Wednesday's storm. In some areas this buried a new layer of surface hoar present on all aspects and elevations. The new snow adds to 100-200 cm of storm snow from the past two weeks, which sits on an unstable snowpack with four other active weak layers:1) 150 to 270 cm of snow sits on the crust and/or surface hoar layer from mid-January. The crust is reportedly widespread, except for possibly high elevation north aspects. The surface hoar was reported up to tree line elevations and possibly higher.2) The early-January weak layer is 170 to 300 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.3) Another weak layer buried mid-December consists of a facet/surface hoar/crust combination, which is buried 200 cm or more below the surface. It is most problematic at and below tree line.4) A crust/facet layer from late November is yet another failure plane responsible for recent very large avalanches.The wide distribution and ongoing reactivity of these layers suggests that choosing simple terrain free of overhead hazard is the best avoidance strategy.

Problems

Storm Slabs

An icon showing Storm Slabs
Heavy snowfall and steady winds have formed reactive new storm slabs on the surface. As the new snow consolidates, potential for human triggering storm slabs will increase. Strong solar effect may act as a trigger for natural avalanches on Friday.
If triggered, storm slabs may step down to deeper layers and result in very large avalanches.Choose low-angled, sheltered terrain where new snow hasn't been wind-affected.Avoid exposure to sun-exposed slopes.

Aspects: All aspects.

Elevations: All elevations.

Likelihood

Very Likely

Expected Size

1 - 3

Persistent Slabs

An icon showing Persistent Slabs
Several unstable weak layers are lurking deep in our snowpack. These layers have the potential to be triggered both naturally and with skier or rider traffic. When triggered, these layers have been producing very large avalanches that can run far.
Avoid the runout zones of avalanche paths. Avalanches could run full path.Use conservative route selection. Choose low-angle, supported terrain with low consequence.

Aspects: All aspects.

Elevations: All elevations.

Likelihood

Likely

Expected Size

2.5 - 4

Valid until: Feb 9th, 2018 2:00PM