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Avalanche Forecast

Archived

Dec 9th, 2021–Dec 10th, 2021

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

Regions

Northwest Inland.

Danger has increased as wind and new snow form fresh wind slabs throughout the day. Seek out wind sheltered terrain where you can avoid these wind slabs and find great riding. 

Confidence

Moderate - Uncertainty is due to the limited number of field observations. Uncertainty is due to the fact that deep persistent slabs are particularly difficult to forecast.

Weather Forecast

Thursday Overnight: Winds increasing strong to extreme from the southwest as the front moves into the northwest ranges. Light to moderate precipitation overnight with 5-10cm of accumulation. Freezing levels at valley bottom with alpine temperatures around -12 C. 

Friday: A stormy day. Strong to extreme southwest winds with moderate to heavy precipitation, 15-30cm of accumulation. Freezing levels rising to around 500m, alpine temperatures around -8 C. 

Saturday: Cloudy with continued light precipitation. Winds easing to moderate to strong from the southwest at ridgetop. Freezing levels at valley bottom with alpine temperatures around -15 C. 

Sunday: Mainly cloudy with scattered flurries, 2-5 cm accumulation. Moderate westerly winds at ridgetop, alpine temperatures around -15 C. 

Avalanche Summary

On Saturday, a size 3 avalanche was reported in the Hankin-Evelyn area, failing near the ground. This has us thinking about the potential for a deep persistent weak layer.

On Thursday, our field team was out in the Telkwa mountains, they saw a few natural cornice failures up to size 2. Keep in mind that cornice failures have the potential to put a large load on the snowpack and trigger deeper layers.

If you do head out in the backcountry, please share your observations to the Mountain Information Network!

Snowpack Summary

Up to 40 cm of new snow has fallen in the past week with another 10-20 cm expected throughout the day today. Strong to extreme southwest winds will redistribute this new snow into new wind slabs in the alpine and treeline. These new wind slabs will overlie older wind slabs from earlier in the week, amongst a variety of hard, wind effected surfaces. 

Below 1400m, a thin rain crust exists below the new snow. There have been reports of faceting around this crust with recent cold temperatures. A spotty surface hoar layer has been reported down ~100cm in the alpine and treeline. 

An early season crust can be found near the base of the snowpack. It has shown reactivity in the past week with large loads (explosives and cornice), creating large avalanches. We don't know how widespread this problem may be. With the incoming snow and wind we are definitely keeping an eye on it, and would be avoiding large features and areas with thin to thick snowpack transitions.

Snowpack depth at treeline ranges from 150-200 cm, with higher values in the western part of the region, tapering to the east.

Terrain and Travel

  • Avoid shallow, rocky areas where the snowpack transitions from thick to thin.
  • Look for signs of instability: whumphing, hollow sounds, shooting cracks, and recent avalanches.
  • Seek out sheltered terrain where new snow hasn't been wind-affected.

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.