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Avalanche Forecast

Archived

Feb 26th, 2021–Feb 27th, 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 unlikely, human triggered possible.
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, human triggered possible.

Regions

Cariboos.

The snowpack in the Cariboos is complex. Stick to simple terrain and resist the urge to venture into bigger terrain, now is not the time to get after it!

Confidence

Moderate - Uncertainty is due to the complexity of the snowpack’s structure. Uncertainty is due to the fact that persistent slabs are particularly difficult to forecast.

Weather Forecast

FRIDAY NIGHT - Cloudy with clear periods / light to moderate northwest wind / alpine low temperature near -14 

SATURDAY - A mix of sun and cloud / light to moderate northwest wind / alpine high temperature near -13

SUNDAY - Mainly cloudy with a few flurries / strong southwest wind / alpine high temperature near -6 / freezing level 1500 m

MONDAY - Flurries, 5-10 cm / strong southwest wind / alpine high temperature near -7 / freezing level 1300 m

Avalanche Summary

There was a widespread natural avalanche cycle ongoing during the stormy weather. Natural avalanche activity will likely decrease on Saturday with cool, dry weather. However, the potential exists for large avalanches on deeply buried weak layers. Low-angle terrain choices will be the key to managing this possibility.

There was a report of a natural size 2.5 avalanche running full path in the Dore River area on Thursday. A MIN report about this can be viewed here.

Several natural and human-triggered avalanches size 2-3.5 were reported on Tuesday near Valemount at alpine and treeline elevations. At least one of the very large human-triggered avalanches was initiated from a wind-loaded start zone at the top of a large alpine feature, propagated for hundreds of meters along a ridge, and ran to valley bottom. Thankfully the rider was able to escape unharmed.

On Tuesday, there was a fatal avalanche just outside of the region, northeast of Valemount in Swift Creek. The avalanche was a size 3.5 and is suspected to have failed on the late January persistent weak layer. The report can be found here.

Snowpack Summary

The region has received 40-80 cm of fresh snow in recent days. There are deep wind deposits in lee features at upper elevations. The recent snow sits on a persistent weak layer of facets that formed on the surface during the recent cold snap.

There is now 80-180 cm of snow above another persistent weak layer from early February which is composed of surface hoar. This layer is most prevalent at treeline and below treeline. On steep south-facing terrain, this layer may consist of facets on a sun crust. 

Yet another persistent weak layer from late January exists down 90-200 cm. There have been very few recent reports of avalanches or reactive test results on this layer, however, there have been several large avalanches on this layer in the neighboring North Rockies region recently, so it is worth keeping in mind.

Terrain and Travel

  • Use conservative route selection and resist venturing out into complex terrain.
  • Fresh snow rests on a problematic persistent slab, don't let good riding lure you into complacency.
  • Be aware of the potential for large avalanches due to the presence of a persistent slab.
  • Be especially cautious as you transition into wind affected terrain.
  • Brief periods of sun could quickly initiate natural avalanche activity.

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.