Avalanche Forecast

Issued: Mar 7th, 2020 5:00PM

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

Avalanche Canada astclair, Avalanche Canada

Email

The snowpack cannot be trusted right now. Large, human-triggered avalanches on a buried weak layer are likely. A conservative mindset and terrain use strategy is critical for Sunday.

Summary

Confidence

High -

Weather Forecast

Saturday night: Clearing overnight, scattered flurries with up to 5 cm of snow, light southwest wind, alpine temperature -10 C.

Sunday: Mostly cloudy, convective flurries with up to 5 cm of snow, light southwest winds, alpine high temperature -5 C.

Monday: Mostly clear, light southwest wind, alpine high temperature -5 C, freezing level 1200 m. 

Tuesday: Increasing cloud, isolated flurries with trace accumulations, alpine high temperature -4 C, freezing level 1400 m.

Avalanche Summary

Consistent reports of avalanches releasing on the February 22 surface hoar have been submitted over the past week. Human-triggered and remotely-triggered avalanches have been reported, even as professionals tiptoe around and avoid suspect terrain features. The problem is touchy but tricky. In many instances, slopes were ski cut with no results, only to have the third or fourth skier in the group trigger the slab. These avalanches have propagated widely across terrain features, warranting conservative terrain margins (see this MIN for a helpful example). Avalanche size has increased over the past several days, with more of the activity releasing size 2+. Observations extend to all aspects and elevations, but north to east aspects near treeline have been a hot-spot for reactivity. Avalanches are also occurring at unusually high elevations for surface hoar.  

Several small to large (size 1-2) natural and human-triggered avalanches have been observed breaking in the recent storm snow. A few large (size 2) cornices were also observed failing naturally. If triggered, wind slabs and cornice falls could step down to the buried surface hoar layer, forming large avalanches. Use added caution on sun-exposed slopes when the sun is shining, as it could rapidly deteriorate the storm snow and cornices and cause loose or slab avalanches.

On Thursday, professionals reported large (size 2.5) explosive triggered avalanches releasing on weak layers near the ground. These avalanches occurred on north and east facing slopes above 2300 m, and they confirm that this problem remains a concern. 

Snowpack Summary

Snowfall amounts varied across the region on Saturday, with the highest totals falling in the southern part of the region. Slab formation and human triggering will likely be specific to where the wind has transported the snow into deeper drifts.

A weak layer of surface hoar from February 22 may be found 35-70 cm deep. It may sit over a crust on solar aspects. With successive storms, more areas have reached critical loading and developed a slab over this layer. Riders will be capable of triggering this layer for some time until there is a substantial change in the snowpack. Read more about surface hoar on our forecaster blog.

Deep basal facets lurk near the bottom of the snowpack. This layer has been responsible for sporadic deep persistent slab avalanches, usually triggered from shallow, rocky start zones.

Terrain and Travel

  • It's critical to stay disciplined and choose only well supported, low consequence lines.
  • Be aware of the potential for large avalanches due to the presence of buried surface hoar.
  • Stay off recently wind loaded slopes until they have had a chance to stabilize.
  • Avoid shallow, rocky areas where the snowpack transitions from thick to thin.

Problems

Persistent Slabs

An icon showing Persistent Slabs

A weak layer of surface hoar sits 35-70 cm deep, within the prime range for human-triggering. Over the past several days, large human-triggered and remotely-triggered avalanches have released on this layer. Avalanche activity is expected to become more likely and widespread, as more areas approach critical loading from the recent snow. 

Aspects: All aspects.

Elevations: All elevations.

Likelihood

Likely

Expected Size

1 - 2.5

Wind Slabs

An icon showing Wind Slabs

Incremental snowfall with wind has formed wind slabs in the alpine and open areas at treeline.This problem also overlaps with where cornices may be reaching their breaking point. If triggered, wind slabs and cornices could step down to the buried surface hoar layer, forming large avalanches. Use added caution on sun-exposed slopes when the sun is shining, as it could rapidly deteriorate the storm snow and cornices and cause loose or slab avalanches.

Aspects: North, North East, East, South East, South, North West.

Elevations: Alpine, Treeline.

Likelihood

Possible - Likely

Expected Size

1 - 2

Deep Persistent Slabs

An icon showing Deep Persistent Slabs

Weak snow at the bottom of the snowpack continues to pose a deep persistent slab avalanche problem. Treat wind-scoured, rocky, shallow terrain as suspect and avoid big alpine slopes that are threatened by cornices overhead. 

Aspects: All aspects.

Elevations: Alpine, Treeline.

Likelihood

Unlikely - Possible

Expected Size

2 - 3.5

Valid until: Mar 8th, 2020 4:00PM

Login