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Avalanche Forecast

Archived

Feb 6th, 2022–Feb 7th, 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 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 possible, human triggered probable.

Regions

South Columbia.

It is uncertain how reactive the recently buried weak layer is to human triggers. Once triggered, it will likely result in a large avalanche that can have serious consequences. This 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

SUNDAY NIGHT: Clear with increasing clouds, light to moderate southwest wind, alpine temperature +1 C, above freezing layer from 1600 m to 2500 m. 

MONDAY: Mix of sun and cloud, up to 5 cm new snow, moderate to strong west wind, alpine temperature -2 C, the above freezing layer will be pushed out Monday morning, freezing level dropping to 1500 m.

TUESDAY: Mix of sun and cloud, up to 3 cm new snow, light west wind, alpine temperature -5 C, freezing level 1400 m.

WEDNESDAY: Cloudy, up to 5 cm new snow, light west wind, alpine temperature-2 C, freezing level rising to 2100 m. 

Avalanche Summary

On Sunday, at the time of writing, explosives triggered numerous storm slabs up to size 2 below treeline on southeast aspects.

On Saturday, several large natural storm and wind slabs up to size 3 were observed on all aspects in the alpine. Explosives triggered avalanches up to size 2.5. Riders triggered many small wind slabs up to size 1.5 at treeline as well as a large (size 3) wind slab in the north of the region (see this MIN report). Many avalanches released on the weak layer that was buried at the end of January. 

On Friday, a natural avalanche cycle of storm slabs up to size 2 was observed, as well as a large size 3 avalanche on an east aspect. Numerous small rider triggered avalanches and a large (size 2) storm slab triggered by a skier were reported. Explosives triggered numerous large (size 2) avalanches. A deep persistent slab avalanche was triggered by a machine and released on the early December facet/crust layer described in the Snowpack Summary.

Many storm and wind slabs were triggered by riders on Thursday to add to the many avalanches observed in the previous few days. Most of the storm slabs released on the surface hoar layer described in the Snowpack Summary, often occurring between around 1600 and 2200 m on all aspects except due south. Read this MIN for a detailed description of a skier-triggered avalanche in the south of the region -- thank you for the detailed report.

Snowpack Summary

The recent storm brought 10 to 30 cm snow. The snow has formed storm slabs in areas sheltered from the wind and wind slabs in exposed terrain at higher elevations from strong south to southwest wind. 

The snow loaded a weak layer of surface hoar crystals 5 to 15 mm in size. Warm temperatures overnight Sunday to Monday will keep the likelihood of triggering a slab increased. The layer may be around 40 to 80 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 100 to 240 cm. The last reported avalanche was on February 4 in the southwest of the region. 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

  • Shooting cracks, whumphs and recent avalanches are strong indicators of an unstable snowpack.
  • Be aware of the potential for larger than expected storm slabs due to the presence of buried surface hoar.
  • 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.

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.