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Avalanche Forecast

Archived

Feb 18th, 2022–Feb 19th, 2022

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

Regions

North Columbia.

Greatest snowfall amounts are forecast for the Monashees, where touchy storm slabs will build with heavy snowfall throughout the day.

Concern for a buried weak layer necessitates conservative terrain travel. Be aware of above and adjacent slopes.

Confidence

Moderate - Forecast precipitation (either snow or rain) amounts are uncertain. Uncertainty is due to the fact that persistent slabs are particularly difficult to forecast.

Weather Forecast

Precipitation will begin on Friday evening, as a frontal system enters the region from the north. Moderate to heavy snowfall is forecast for Saturday, with a clearing trend forecast for early next week.

Friday Overnight: Cloudy with light precipitation, trace to 15 cm of new snow accumulation at higher elevations. Freezing level around 1500 m. Moderate to strong southwesterly winds. 

Saturday: A stormy day with moderate to heavy snowfall, 10-30 cm of accumulation. Freezing level around 1000 m. Moderate to strong southwesterly winds. 

Sunday: A mix of sun and cloud with light snowfall. Freezing level at valley bottom with alpine temperatures around -10 C. Light to moderate northwesterly winds.

Monday: Mainly clear. Alpine temperatures plummeting into the -20s. Light northeasterly winds. 

Avalanche Summary

Natural and human-triggered storm slabs are likely on Saturday.

On Wednesday, we received numerous reports of reactive wind slab avalanches mostly up to size 1.5 and several larger ones up to 2.5 from alpine features. These wind slabs ran naturally and were easily triggered by the weight of a skier. Explosive control also initiated some larger persistent slabs up to size 2.5.

Last week, near-daily reports came in of human-triggered persistent slab avalanches on the January 30th weak layer, with the associated surface hoar layer taking both recreationists and professionals by surprise. The most reactivity on this layer has been seen between 1600-2200 m in open areas in the trees, in cut blocks, and on steep convexities. Reactivity has tapered, but we would continue to be cautious as the snowpack is tested with new load.

Snowpack Summary

Continued snowfall throughout Saturday will add to 10-25 cm of recent storm snow above the old hard surface. This old surface is comprised of near-surface faceting, and in some areas surface hoar growth overlying a melt-freeze crust at lower elevations, a sun-crust on steep solar aspects, and hard wind-affected snow in the alpine and exposed treeline.

Several weak layers exist in the upper snowpack including buried crusts, facets, and a prominent weak layer of buried surface hoar. This surface hoar has been the dominating feature in the past few weeks and is most prominent in sheltered openings at and below treeline. It was buried in late January and exists 50 to 100 cm deep in the snowpack. Reactivity on this layer has begun to taper, but significant snowfall on Saturday could be enough to wake this layer up, initiating large and surprising avalanches. 

The facet/crust layer that formed in early December is now buried around 120 to 250 cm. The last reported avalanche was on January 31 from a large explosive, and before that on January 23. Although unlikely, the layer could be triggered from a large load like a cornice fall or a shallower slab avalanche could step down to this layer. 

Terrain and Travel

  • Storm snow and wind is forming touchy slabs. Use caution in lee areas in the alpine and treeline.
  • Shooting cracks, whumphs and recent avalanches are strong indicators of an unstable snowpack.
  • Be aware of the potential for large avalanches due to the presence of buried surface hoar.
  • Surface hoar distribution is highly variable. Avoid generalizing your observations.

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.