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Avalanche Forecast

Archived

Feb 7th, 2022–Feb 8th, 2022

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

Regions

Purcells.

Wind slabs are expected to remain reactive in exposed high elevation terrain on Tuesday. It may still be possible to trigger a buried weak layer in some areas at and below treeline but the likelihood is decreasing with the cooler weather.

Confidence

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

Weather Forecast

Dry and mainly sunny conditions are expected for the week except for a weak disturbance Tuesday night which may bring light flurries. A major warming event is current forecast to arrive late Wednesday which may persist for several days. 

Monday Night: Lingering flurries in the north, partly cloudy in the south, light to moderate W wind, freezing level dropping to valley bottom.

Tuesday: A mix of sun and cloud with a chance of flurries overnight, light to moderate W wind, freezing levels reaching around 1400 m.

Wednesday: A mix of sun and cloud, moderate NW wind, freezing levels climbing to around 2000 m.

Thursday: Mainly sunny, light to moderate W wind, freezing levels reaching over 2500 m with an inversion.

Avalanche Summary

On Sunday, several natural wind slabs and loose avalanches were reported. A skier remotely triggered a size 1.5 wind slab from 3 m away on an east aspect at 2500 m. Explosives triggered a number of slab avalanches size 1.5-2.5 in the deeper west part of the region where the slab thickness was typically 30-50 cm and up to 120 cm in wind loaded terrain. 

This MIN post from the Dogtooth shows the type of open slopes where the buried surface hoar may be reactive at lower elevations. 

On Saturday, several natural wind slabs up to size 1.5 were reported throughout the region. Ski cuts triggered a couple small slabs and some small loose avalanches in steep terrain. A skier remotely triggered a size 1.5 slab from 5 m away on a west aspect at 1900 m which failed on the late-January surface hoar down 55 cm in the deeper western part of the region. Explosives triggered a size 2 cornice which released a slab on the slope below. 

Snowpack Summary

A new sun crust is being reported on solar aspects into the alpine and a temperature crust on all aspects at lower elevations. Ongoing periods of strong wind from the southwest through northwest have formed reactive wind slabs in exposed terrain at higher elevations. 

The January 30 interface is now typically down 20-40 cm and consists of a melt-freeze crust at lower elevations and on solar aspects extending into the alpine, surface hoar in sheltered areas at and below treeline, and small facets in some areas.

Several old surface hoar layers are now buried in the upper snowpack 40-70 cm deep. While these old layers appear to have gone dormant, there is still an isolated chance of avalanches stepping down to a deeper layer. 

The early December crust/facet layer of concern sits around 80 cm deep in the eastern Purcells and shallow terrain, and up to 150 cm in the west. This layer produced numerous large avalanches in January but is now considered dormant. See this forecaster blog on how to manage this layer as it may come into play again later this season. 

Terrain and Travel

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Be aware of the potential for large avalanches due to the presence of buried weak layers.
  • Look for signs of instability: whumphing, hollow sounds, shooting cracks, and recent avalanches.

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.