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Avalanche Forecast

Archived

Dec 14th, 2021–Dec 15th, 2021

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

Regions

Purcells.

Adopt a conservative approach to choosing terrain, and avoid thin, rocky start zones. The snowpack appears to be gaining strength, but some persisting weak layers could still be reactive to a rider's weight.

Confidence

Moderate - We are confident about the possible sizes of avalanches, should one release; what is less certain is the likelihood of triggering.

Weather Forecast

The cloud and intermittent light flurries are continuing to hang with us, with some possible clear periods on the drier, east side of the mountain range. The southeast corner of the region may see stronger winds at treeline and above.

TUESDAY NIGHT: Mix of sun and cloud, clearer on the eastern slopes. 0-5 cm of snow expected. Moderate southwest winds. Freezing level falling to valley bottom. 

WEDNESDAY: Mix of sun and cloud, clearer on the eastern slopes. Possible trace of snow. Light to moderate southwest winds, westerly at higher elevations. Alpine temperatures around -12

THURSDAY: Partly cloudy. 0-2 cm of snow expected. Light southwest wind, trending to strong northwest at higher elevations in the afternoon. Alpine temperatures cooling to around -14.

FRIDAY: Clearing with isolated clouds. No new snow expected. Light southwest winds, trending to strong northwest in the alpine. Alpine temperatures around -11 with a possible temperature inversion setting up. 

Avalanche Summary

No new natural avalanches were reported.

Yesterday, avalanche control in the north of the region produced very small avalanches in the storm snow, and on Monday, small, skier triggered avalanches on north aspects.

On Sunday, a small, skier remote triggered avalanche was reported that failed on a reloaded bed surface near the base of the snowpack on a north aspect in the alpine. There were other deep failures reported in this region about a week ago. This information is spotty, but it is consistent with a deep persistent problem that may be difficult to trigger. We're not done worrying about this one yet.

Snowpack Summary

Other than some strong southwest alpine winds potentially forming new windslabs, the snowpack likely remains fairly unchanged from yesterday.

 

Variable snowfall over the region Monday night added up to 15cm of low density snow to the top of the snowpack. This snow fell with mostly light winds, so there should have been very little new slab formation. 

Recently, moderate to strong southwest winds redistributed the previous storm's snow over the early December rain crust. This crust should be a very obvious feature 40-80 cm down from the snow surface. It is 10-40 cm thick, and can be found on all aspects up to 2300m. 

This thick crust is likely to encourage facet formation above and below itself, so it will remain a layer to watch. 

A late October facet/crust layer of concern sits at the bottom of the snowpack above 1900m. This layer has been reactive to human triggers, producing large avalanches. This layer is widespread and will likely continue to be a layer of concern.

Snowpack depth at treeline is 115-200cm, with the deepest snowpack found near the Bugaboos. 

Terrain and Travel

  • Use conservative route selection and resist venturing out into complex terrain.
  • Be alert to conditions that change with elevation and wind exposure.
  • Avoid thin areas like rock outcroppings where you're most likely to trigger avalanches failing on deep weak layers.

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.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.