Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Feb 24th, 2020–Feb 26th, 2020

Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.

Regions

North Rockies.

Conservative terrain decisions are recommended as it remains possible to trigger large avalanches on buried surface hoar. New slabs will form throughout the week with the arrival of snow, wind, and mild temperatures. 

Confidence

Moderate - Forecast snowfall amounts are uncertain.

Weather Forecast

Stormy weather will return Tuesday afternoon and continue throughout the week.

MONDAY NIGHT: Mostly cloudy, moderate west wind, alpine temperatures drop to -12 C.

TUESDAY: Increasing cloud with snow starting early afternoon, 5-10 cm along western side of the divide and 2-5 cm along the eastern side, strong southwest wind with gusts up to 70 km/h, alpine high temperature around -6 C.

WEDNESDAY: Scattered flurries with 5-20 cm of new snow, strong southwest wind, freezing level climbs to 1200 m with alpine high temperatures around -3 C.

THURSDAY: Isolated flurries with some sunny breaks in the afternoon, strong southwest wind, freezing level climbing to 1500 m, alpine high temperatures around -2 C.

Avalanche Summary

Over the weekend two large (size 2.5) persistent slab avalanches were reported on northeast slopes at Bijoux (see the Mountain Information Network report for photos). One appeared to be triggered by a snowmobile, while the other was triggered naturally by a cornice fall. Similar persistent slab avalanche activity was reported last week on buried surface hoar layers up to 100 cm below the surface. Some natural wind slab avalanches were also observed in alpine terrain, but may have been a few days old.

In areas where buried surface hoar exists, triggering large persistent slab avalanches will remain a concern this week. Otherwise accumulations of snow will form new storm and wind slabs. Cornices will become an increasing concern as temperatures warm up later this week.

Snowpack Summary

The snowpack is currently heavily wind affected in open areas and crusty at low elevations and on south and west facing slopes, but if you're lucky, you can still find powder in sheltered terrain. 

A weak layer of surface hoar buried about 50 cm below the surface has been a problem around Pine Pass and has also been observed in other parts of the region, such as Torpy, but seems to be less of a problem further south towards McBride. It's now sufficiently deep to result in a large avalanche if triggered, so this layer should be factored into your decision-making process, especially when it is getting stressed by snowfall or warming temperatures.

The mid-and lower snowpack layers are generally well-bonded, except for shallow and/or rocky start zones which could harbour weak basal snowpack layers. 

Terrain and Travel

  • Watch for signs of instability like whumpfing, hollow sounds, shooting cracks or recent avalanches.
  • Avoid freshly wind loaded features, especially near ridge crests, roll-overs and in steep terrain.
  • Approach steep open slopes at and below treeline cautiously, buried surface hoar may exist.
  • Caution around slopes that are exposed to cornices overhead.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.