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Avalanche Forecast

Archived

Feb 8th, 2022–Feb 9th, 2022

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

Regions

North Columbia.

Warming and new snow will increase the likelihood of triggering the buried weak layer where it is present. The uncertainty is best managed with conservative terrain choices.

Confidence

Moderate - Uncertainty is due to the fact that persistent slabs are particularly difficult to forecast.

Weather Forecast

TUESDAY NIGHT: Cloudy with snowfall, 5 to 10 cm new snow, light to moderate southwest wind, alpine temperature -5 C, freezing level 1100 m. 

WEDNESDAY: Cloudy with snowfall, up to 5 cm new snow, light to moderate southwest wind, alpine temperature -1 C, freezing level rising to 1900 m. 

THURSDAY: Mix of sun and cloud, up to 3 cm new snow, light to moderate westerly wind, alpine temperature +1 C, freezing level 2300 m. 

FRIDAY: Sunny, light to moderate northwest wind, alpine temperature -7 C, freezing level 1000 m.

Avalanche Summary

On Monday, skiers triggered slabs on the buried weak layer about 60-80 cm deep. Large wind slab avalanches up to size 3 released naturally. Explosives triggered wet loose avalanches up to size 2. 

On Sunday, several avalanches released on the buried weak layer with surface hoar crystals and surprised riders. A few large avalanches (up to size 2.5) released naturally on that same layer. Check out some good example photos here. Small storm slab avalanches were reported on east and southeast facing slopes. Numerous loose wet and loose dry avalanches were triggered by the sun on steep slopes and reached large sizes. A deep persistent slab avalanche was likely triggered naturally by intense warming and sun and released on depth hoar or the November crust. It occurred just north of the region (see this MIN report). 

On Saturday, numerous natural storm and wind slab avalanches up to size 2.5 at all elevations and aspects were reported. Explosives triggered several avalanches up to size 2.5. Skiers triggered a few slab avalanches up to size 2. A large (size 2) avalanche was triggered by skiers from a distance, which likely released on the buried weak layer (see this MIN report). A few small slab avalanches (up to size 1.5) released on that same layer naturally. 

Snowpack Summary

The recent storm brought 20 to 40 cm with locally higher amounts. The snow has formed wind slabs in exposed terrain at higher elevations from strong and extreme south to southwest wind. A sun crust formed on sun-exposed slopes at all elevations. 

The snow loaded a weak layer of surface hoar crystals 5 to 15 mm in size. The layer may be around 60 to 100 cm deep, which is a prime depth for human triggering. The layer is most prominent in areas sheltered from the wind. Example terrain features to treat as suspect include the lee side of protected ridges, openings in the trees, cut blocks, and burns. The layer may not exist on steep sun-exposed slopes, where a melt-freeze crust may be found instead.

The facet/crust layer that formed in early December is 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. Humans are unlikely to trigger it, with perhaps the exception in thin, shallow snowpack areas. Check out the forecaster blog for more information.

Terrain and Travel

  • Be aware of the potential for large avalanches due to the presence of buried surface hoar.
  • Shooting cracks, whumphs and recent avalanches are strong indicators of an unstable snowpack.
  • Uncertainty is best managed through conservative terrain choices at this time.

Problems

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.

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.

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.