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Avalanche Forecast

Archived

Feb 7th, 2021–Feb 8th, 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 unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

South Columbia.

Triggering large avalanches remains likely in wind-drifted snow or on open glades near treeline where a buried weak layer persists. Persistent slab avalanches can travel far and can be difficult to predict, so a conservative approach is recommended. 

Confidence

Moderate - Uncertainty is due to the fact that persistent slabs are particularly difficult to forecast.

Weather Forecast

Brrrrrr! Cold and dry conditions persist under arctic air

Sunday night: Partly cloudy, light northwest wind, alpine temperature -18 C.

Monday: Mainly sunny, light northwest wind, alpine high temperature -20 C.

Tuesday: Mainly sunny, light northwest wind, alpine high temperature -23 C. 

Wednesday: Mainly sunny, light northwest wind, alpine high temperature -23 C.  

Avalanche Summary

Travelers may encounter three different flavors of avalanches on Monday. Expect loose dry avalanches in steep areas where the recent snow has not formed a slab. Although typically small (size 1-1.5), these avalanches pose a serious concern for ice climbers and for people traveling in extreme terrain where the possibility of getting knocked off of your feet has severe consequences. At upper elevations, newly formed wind slabs are expected to be reactive to human triggering. At treeline elevations and below, avalanches may be remotely triggered and break larger than expected on a reactive layer of surface hoar.

Over the past 48 hours, numerous large (size 2-2.5) natural, human, and explosive triggered wind slab avalanches have been reported. These avalanches released on north through east through south aspects above 2000 m and broke 30-80 cm deep. 

Over the past week, there have been steady reports of large to very large (size 2-3) skier-triggered persistent slab avalanches, failing on a weak layer of surface hoar down 80-130 cm. This MIN report from Friday in the south of the region near Retallack is a helpful example of where this problem exists in the terrain. This MIN report from earlier in the week near Kokanee Pass offers a sobering look at the potential for this problem to propagate widely across features.

Snowpack Summary

Another 10-15cm of snow and moderate ridgetop winds from the northwest have continued to build wind slabs in lee features at upper elevations. With up to 40 cm of low density snow from the past couple days, cohesion-less snow in sheltered areas may be prone to dry loose avalanches that can run far and fast in these cold, dry conditions.

The snow from the past week is settling over a reactive weak layer of surface hoar buried 80-130 cm deep. This persistent weak layer has potential to surprise backcountry users with how wide the fracture can travel across slopes. Recent avalanches on this layer have primarily been reported at treeline and below, with much of the notable activity coming from areas south in the region. This layer will be slow to gain strength and requires careful terrain selection.

A less reactive layer of surface hoar or facets buried in early January can be found down 100-160 cm.

The mid/lower snowpack is generally well settled and strong in most areas.

Terrain and Travel

  • Avoid open slopes and convex rolls at and below treeline where buried surface hoar may be preserved.
  • Stay off recently wind loaded slopes until they have had a chance to stabilize.
  • Be aware of the potential for loose avalanches in steep terrain where snow hasn't formed a slab.

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.