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Avalanche Forecast

Archived

Feb 27th, 2022–Feb 28th, 2022

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

Avalanche danger will increase throughout the day with heavy snowfall, southwest wind and rising freezing levels. 

Avoid avalanche terrain during periods of heavy loading from new snow and wind.

Confidence

Moderate - Uncertainty is due to the timing, track, & intensity of the incoming weather system. We are confident the likelihood of avalanche will increase with the arrival of the forecast weather.

Weather Forecast

There is some model disagreement around the timing and intensity of the next system. 

Sunday night: Snowfall 5-10 cm, moderate southwest wind, treeline low around -5 °C.

Monday: Snowfall 20-35 cm, moderate to strong southwest wind, rising freezing levels, treeline high around -1 °C.

Monday night: Heavy snowfall possible (up to 50 cm), moderate to strong southwest winds, freezing levels rising into Tuesday morning.

Tuesday: Precipitation continues with 10-15 mm, moderate to strong southwest wind, freezing levels hovering around 2000 m. 

Wednesday: Light snow, light to moderate southwest wind, freezing levels around 1700 m.

Avalanche Summary

On Saturday the wind triggered some small dry loose avalanches and wind slabs were starting to form again in spill zones. No new avalanches were reported on Thursday or Friday. On Wednesday, skiers were triggering small wind slabs. The Avalanche Canada field team reported whumpfing and cracking in places where the late-January surface hoar is still preserved and reactive, but they didn't see any new avalanches.

Last Saturday, there was a machine-triggered persistent slab avalanche on a surface hoar layer in an open gully feature in the Rolling Hills area.

Snowpack Summary

New storm snow will build slabs on a variety of old surfaces like recent wind slabs, sun crusts on south-facing terrain, and cold weak crystals on shaded aspects. 

A buried surface hoar layer that was 30-60 cm deep before the storm can still be found on sheltered, north-facing treeline-type features. This distribution of this layer is spotty in nature but has produced avalanches and snowpack test results in the past week, mostly in the Flathead. While it does not appear to be as widespread or reactive in the Lizard Range, it has been found in some locations. 

The lower snowpack is well consolidated, with a crust/facet layer from early-December found near the bottom of the snowpack. It is currently considered dormant but could become active later this season. Check out the forecaster blog for more information. 

Terrain and Travel

  • Storm slab size and sensitivity to triggering will likely increase through the day.
  • Avoid all avalanche terrain during periods of heavy loading from new snow and wind.
  • Storm slabs in motion may step down to deeper layers resulting in large avalanches.

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.