Avalanche Forecast

Issued: Mar 1st, 2020 3:00PM

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 ghelgeson, Avalanche Canada

While the persistent slab problem is becoming a bit less sensitive to triggering, last week's snow and wind has activated the deep persistent slab, the potential for these large destructive avalanches needs to be accounted for in your travel plans. 

Summary

Confidence

Moderate - Uncertainty is due to the fact that deep persistent slabs are particularly difficult to forecast. Uncertainty is due to the timing, track, & intensity of the incoming weather system.

Weather Forecast

Out of the frying pan and into the fire, it looks like we’re in for another series of significant storms this week.

SUNDAY NIGHT: Freezing level around 1000 m, strong to extreme west/northwest wind, 1 to 5 cm of snow possible.

MONDAY: Overcast, freezing level rising to about 1000 m, strong west/northwest wind, 1 to 3 cm of snow possible during the day, 3 to 10 cm of snow possible Monday night.

TUESDAY: Broken cloud cover, freezing level around 800 m, moderate southwest wind, 1 to 5 cm of snow possible during the day, 1 to 5 cm of snow possible Tuesday night.

WEDNESDAY: Broken cloud cover, freezing level beginning at valley bottom rising to 600 m, moderate west/southwest wind, trace of snow possible.

Avalanche Summary

It's been an active period for avalanche activity:

On Saturday a human triggered size 1 was reported on a northeast facing slope at 1500 m, failing on the Feb. 19th surface hoar. There was a great MIN report from Ashman too that shows some shallow slab avalanches.

On Friday a natural cornice failure produced a size 3.5 deep persistent slab on a northeast facing feature at 1800 indicating that the deep persistent slab problem continues to be active. Human triggered wind slab avalanches up to 30 cm in depth were running on the February 19th surface hoar too.

On Thursday natural avalanches to size 2 were observed running on the February 19th surface hoar.

Some very large and destructive avalanches have been sporadically running on deeply buried weak layers near the bottom of the snowpack, predominantly on north through east aspects in the alpine. On February 17 and 18 there were three large (size 2.5-3) deep persistent slab avalanches in thin rocky terrain. Steady loading last week once again aggravated these deeper layers. 

Snowpack Summary

A few cm fell Sunday which may preserve yet another layer of surface hoar.

30 to 50+ cm of settled snow overlies the Feb 19 surface hoar in sheltered locations and a sun crust on solar aspects with the deeper slabs being found in the north of the region. The alpine has been heavily wind affected as evidenced by this MIN submission. The surface hoar may be most sensitive to human triggering at treeline which is a bit different setup than we're used to.

There are few different persistent weak layers (PWL's) we're watching in the mid and lower snowpack. A patchy layer of small surface hoar crystals and a sun crust both from early February are now 40 to 100 cm deep. A couple of weak layers that formed in January are buried in proximity to one another 80-140 cm below the surface. Below that, an early season crust lurks at the base of the snowpack. Some large avalanches have been triggered on these layers, usually during periods of rapid loading by new snow or wind and by large loads or from thin, rocky areas. We're now in another one of those periods that could wake up the deep slab.

Terrain and Travel

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Use careful route-finding and stick to moderate slope angles with low consequences.
  • The trees are not the safe-haven they normally are at this time. Terrain at treeline is primed for human triggered avalanches.
  • Surface hoar distribution is highly variable. Avoid generalizing your observations.

Problems

Persistent Slabs

An icon showing Persistent Slabs

30 to 50 cm of settled snow rests on a widespread layer of buried surface hoar. While this weak layer is thought to be present at all elevations, these slabs have been most sensitive to triggering at treeline which is a setup that can catch us off guard. Watch for deeper slabs at ridge crest too.

Aspects: All aspects.

Elevations: All elevations.

Likelihood

Possible - Likely

Expected Size

1 - 2

Wind Slabs

An icon showing Wind Slabs

A bit of new snow and strong wind is expected to form fresh wind slabs which will be most prevalent at upper elevations. Fresh wind slabs in motion could step down to the February 19th surface hoar and release persistent slab avalanches.

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

Elevations: Alpine.

Likelihood

Possible

Expected Size

1 - 2

Deep Persistent Slabs

An icon showing Deep Persistent Slabs

Consistent dribs and drabs of snow last week accompanied by strong southwest wind has aggravated the deep persistent slab problem. Some very large and destructive avalanches have been sporadically failing on deeply buried weak layers, predominantly on north through east aspects in the alpine.

Aspects: All aspects.

Elevations: Alpine, Treeline.

Likelihood

Unlikely - Possible

Expected Size

2.5 - 3.5

Valid until: Mar 2nd, 2020 5:00PM

Login