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Avalanche Forecast

Archived

Dec 8th, 2021–Dec 9th, 2021

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

Regions

North Rockies.

Strong winds will keep danger elevated at higher elevations. There is still some concern around buried weak layers, and conservative terrain travel will be necessary as we obtain more information. 

Confidence

Moderate - Uncertainty is due to the limited number of field observations. Uncertainty is due to the speed, direction, or duration of the wind and its effect on the snowpack.

Weather Forecast

Unstable northwest flow will continue to bring unsettled weather for the next few days. On Friday afternoon, we will start to see the effects of a strong pacific front moving into the northwest ranges.

Wednesday Overnight: A mix up sun and cloud with isolated flurries. 5-10 cm of accumulation overnight. Moderate to strong northwest winds easing slightly and shifting to the west. Freezing levels at valley bottom with alpine temperatures around -15 C. 

Thursday: Partially cloudy with flurries, accumulation up to 5cm. Strong westerly winds at ridgetop and alpine temperatures around -15 C. 

Friday: Mainly cloudy. Strong westerly ridgetop winds increasing throughout the day and shifting to the southwest. 5-10cm of new snow throughout the day with freezing levels rising to 500m.

Saturday: Overnight, freezing levels reaching 1000-1500m and winds peaking in the early morning strong to extreme form the southwest. 10-15cm of new snow throughout the day, tapering into the afternoon.  

Avalanche Summary

Expect natural and rider triggered avalanches to occur as the new snow continues to be redistributed by westerly wind. If you do head out in the backcountry, please share your observations to the Mountain Information Network!

 

Large cornices are looming! There have been several natural cornice failures reported in the Bijoux area on Tuesday. This problem will only increase with continued wind transport. Be aware of what is above you, and consider that cornice failures have the potential to trigger deeper layers.

                                                                                                                                                                                                                                                     

Over the past week, a few large avalanches were observed in the Southeast corner of the region. These avalanches ran on a deep persistent layer, likely one of the crusts from late October or early November.

Snowpack Summary

Yesterday's 15-30cm of new snow will bring the week's total to 30-40cm. In sheltered areas, this new snow will remain loose and unconsolidated, but in exposed areas strong westerly winds will redistribute this snow into fresh wind slabs in the alpine and treeline. 

Prior to this storm, in the south of the region, 5-10mm surface hoar growth has been observed from cold, clear nights on Sunday and Monday. Elsewhere, cold temperatures will have promoted near surface faceting. This will create a weak layer for new wind slabs to fail on, especially where a crust is present below. As a result, extra caution should be taken as we investigate the bond between these layers.

The lower snowpack consists of a series of early season crusts. Cold temperatures will have promoted faceting around these crusts. Shallow alpine slopes along the eastern side of the Rockies towards Jasper may have weaker, faceted snow near the ground. 

Snowpack depths at treeline range from 60cm-200cm, with the shallower value mainly in the eastern side of the range. The alpine snowpack ranges from 150cm-200cm. 

Terrain and Travel

  • Potential for wide propagation exists, fresh slabs may rest on surface hoar, facets and/or crust.
  • Choose conservative terrain and watch for clues of instability.
  • Watch for signs of instability like whumpfing, hollow sounds, shooting cracks or recent avalanches.

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.