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Avalanche Forecast

Archived

Jan 20th, 2022–Jan 21st, 2022

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

Regions

Lizard-Flathead.

The recent storm snow combined with strong winds forecast Friday may form reactive wind slabs.

Be mindful of the lingering deep persistent slab problem. Forecast warming temperatures and sunshine this weekend may be enough to wake this problem up and initiate very large avalanches.

Confidence

Moderate - Uncertainty is due to the timing, track, & intensity of the incoming weather system.

Weather Forecast

A lot of uncertainty exists with the timing and persistence of the warming that is forecast for Saturday onward.

Friday: Mostly cloudy with no new snow and strong westerly ridgetop winds. Alpine temperatures near -6 and freezing levels at the valley bottom.

Saturday: The region may start to see some warming with the potential for an upper inversion (warmer air aloft 1500-2000m) bringing valley clouds and some sunny skies in the alpine. Alpine temperatures near 0 degrees. Below freezing in the valley bottoms.

Sunday: Mix of sun and cloud with isolated flurries. Ridgetop winds light from the West and alpine temperatures near 0 to -1 if the temperature inversion remains. Freezing levels valley bottom.

Avalanche Summary

On Thursday, skier-controlled and loose-dry avalanches up to size 1.5 were reported. 

Wind slabs may form and become reactive on Friday with the new snow and increased ridgetop winds. They may have a poor bond to the underlying crust.

A near-miss happened this weekend on Tombstone mountain when a rider triggered a large persistent slab and got completely buried. Luckily, the airbag helped keep the victim's head above the snow. This evidence suggests the deep persistent slab problem is still a concern in the region.

Snowpack Summary

Up to 15 cm of new storm snow fell Thursday with fairly light winds. Winds are forecast to pick up overnight and into Friday building fresh wind slabs on leeward slopes. Wind slabs may be more reactive where they sit above older wind-affected and crusty surfaces. Around 2000 m and below, a crust caps the dense 15 to 30 cm of snow which has settled significantly with the past mild temperatures. The crust varies from thin and breakable (1800 m and below) to thick and supportive (above 1800 m). Below this, the midpack is well consolidated. 

The most notable layer of concern in the snowpack is a crust that was formed in early December and is now down 100-270 cm. This layer was last reactive on Thursday, Jan 13 with warming. This layer has created a tricky low likelihood, high consequence scenario. However, with warm temperatures forecast this weekend we could see this layer wake up and produce very large and destructive avalanches again.

Terrain and Travel

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Wind slabs may be poorly bonded to the underlying crust.
  • 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 deep persistent 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.

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.