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Avalanche Forecast

Archived

Dec 26th, 2020–Dec 27th, 2020

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

Regions

Northwest Inland.

Strong winds blowing from many directions have created windslabs on a variety of aspects at exposed treeline and above. If triggered - a small slab may step down and trigger a much larger and destructive avalanche.  

Confidence

Moderate - Uncertainty is due to the limited number of field observations. Confidence is due to a stable weather pattern; little change is expected for several days.

Weather Forecast

Mild cool weather for the forecast period with mainly cloudy skies & isolated flurries for Sunday then a mix of sun and clouds as high pressure builds across the region for Monday / Tuesday.  

Saturday night: Mainly cloudy with isolated flurries. Alpine low temperatures near -8C and freezing levels valley bottom. Ridgetop wind light to moderate from the southeast switching to southwest. 

Sunday: Mainly cloudy with isolated flurries. Alpine high temperatures near -6C and freezing levels valley bottom. Ridgetop wind increasing moderate to strong from the southwest. 

Monday: A mix of sun and clouds. Alpine temperatures near -6C and freezing levels valley bottom. Ridgetop wind decreasing to light to moderate from the west. A mild temperature inversion will lead to valley fog with clear warmer temperatures above.

Tuesday: Mainly cloudy with scattered flurries. Alpine low temperatures near -10C and freezing levels valley bottom. Ridgetop wind light to moderate from the southeast. A mild temperature inversion will lead to valley fog with clear warmer temperatures above.

Avalanche Summary

No new reports from recent days.

A MIN report submitted on Tuesday showed a deep release from a leeward high alpine feature off the north side of Hudson Mountain. The deep persistent slab problem may be isolated, however it is very high consequence if you find yourself involved in an avalanche of this size.

Last Sunday a human triggered slab avalanche size 2 was reported near Little Simpson. It appears to have started as a wind slab or storm slab and then stepped down to the early December persistent weak interface. Reports from Dec 19th and Dec 17th continue to highlight the instability of slabs that have formed above the early December rain crust. 

Snowpack Summary

Recent moderate to strong winds and recent snow earlier this week have scoured some areas and have built stiff wind slabs in others. Wind directions have been predominately from the south and east souring south and east aspects and loading lee north and wast aspects. As winds shift back to the west be on the look out for buried windslabs, cross loading or reverse loading patterns. 

While much of the region received 5-15cm in the recent storms, some of the higher more mountains areas may have received up to 30cm. In wind sheltered locations, there is now about 30-70 cm of snow above an early-December melt-freeze crust with weak and sugary faceted grains around it. This layer bay be deeper in deeper snowpack or wind-loaded areas - as reported from Hankin. This early December crust layer has featured in several avalanche reports from Dec 19th and Dec 17th in Hankin. This interface was reactive to human triggering in the last week and produced size 2 avalanches. 

A crust that was buried in early November sits near the base of the snowpack. This crust has weak facets associated with it. These facets have produced large avalanches in both the south and north of the region. This MIN report from December 22 highlights a deep release avalanche and the variable snowpack depths.

Snowpack depths vary substantially with aspect, elevation, and wind exposure.

Terrain and Travel

  • Be careful with wind loaded pockets, especially near ridge crests and roll-overs.
  • If triggered, wind slabs avalanches may step down to deeper layers resulting in larger avalanches.
  • In areas where deep persistent slabs may exist, avoid shallow or variable depth snowpacks and unsupported terrain features.
  • Be aware of the potential for large avalanches due to the presence of a buried crust.

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.

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.