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Avalanche Forecast

Archived

Jan 2nd, 2022–Jan 3rd, 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 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.

Touchy new slabs are expected on Monday as the storm progresses and the region continues to deal with a persistent slab problem.

Southern areas of the region may see larger snowfall amounts. If more than 25 cm of new snow is observed, the hazard should be treated as HIGH.

Confidence

Moderate - Uncertainty is due to the timing, track, & intensity of the incoming weather system.

Weather Forecast

A storm system is forecast to bring substantial snowfall to the south of the region on Sunday night and Monday with strong winds. 

Sunday night: Snowfall 10-15 cm in the south, 5-10 cm in the north, moderate to strong SW wind, treeline temperature around -12 °C. 

Monday: Snowfall 15-20 cm in the south, 5-10 cm in the north, moderate to strong SW wind, treeline high around -10 °C. 

Tuesday: A mix of sun and cloud with a chance of flurries, light to moderate SW wind, treeline high around -10 °C. 

Wednesday: A mix of sun and cloud, light to moderate NW wind, treeline high around -12 °C. 

Avalanche Summary

On Sunday, ski cutting was triggering size 1 wind slabs. No new avalanches were reported on Friday or Saturday. 

There has been consistent reports of persistent slab avalanches on reloaded bed surface crusts from the Invermere area over the past month. On Thursday, a size 1 was triggered remotely by bootpacking on a thin northeast aspect in the alpine. Explosive control work on December 26th produced large avalanches (size 2) on the crust found 40-70 cm deep.

On Monday, new wind slabs are expected to form throughout the region with the incoming storm system and strong winds. In the south of the region, these slabs have the potential to be more widespread. These new slabs will sit on a weak snow surface and may be very reactive. The persistent slab problem remains a serious concern and the weight of the new snow may increase the reactivity of these deeper layers. Smaller storm slab avalanches also have the potential to step down to deeper layers resulting in very large avalanches. 

Snowpack Summary

The new storm snow buries a variable snow surface which is likely very weak and includes widespread facets, wind affected surfaces, and/or surface hoar up to 3 mm in sheltered areas. The new snowfall is expected to be accompanied by strong winds and reactive new slabs are expected to be widespread in the south of the region where the most new snowfall is expected. In the north, new slabs may be more isolated to wind loaded terrain. 

The most notable layer of concern in the snowpack is a crust that was formed in early December and is now down 60-120 cm. Activity on this layer has been sporadic. It has generally been triggered on steep, rocky slopes, with a shallow or thin-to-thick snowpack. This layer has created a low likelihood, high consequence scenario which is best managed through conservative terrain choices and disciplined backcountry travel techniques.

A late October facet/crust layer sits at the bottom of the snowpack above 1900 m. 

Terrain and Travel

  • Storm slab size and sensitivity to triggering will likely increase through the day.
  • Be aware of the potential for large avalanches due to the presence of a persistent slab.
  • Avoid steep, rocky, and wind effected areas where triggering slabs is more likely.

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.