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Avalanche Forecast

Archived

Dec 28th, 2019–Dec 29th, 2019

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

Regions

Sea To Sky.

The persistent slab is evolving to a low probability/high consequence scenario where you may not observe any signs of unstable snow before making a dangerous decision. Managing reactive wind slabs adds further complexity to choosing safe terrain on Sunday.

Confidence

No Rating - We are confident about the possible sizes of avalanches, should one release; what is less certain is the likelihood of triggering. Uncertainty is due to the limited number of field observations.

Weather Forecast

Saturday night: Cloudy with scattered flurries continuing overnight bringing 3-5 cm of new snow, light to moderate southwest winds, alpine high temperatures around -4 C and freezing level near 1000 m.

Sunday: Cloudy with isolated flurries and 1-3 cm of new snow. Light south winds. Alpine high temperatures around -1 C with freezing levels rising to 1800 m.

Monday: Mix of sun and cloud, isolated flurries with 1-3 cm of accumulation possible overnight, light to moderate southwest winds, alpine high temperature near -2 C with freezing levels dropping from 1200 m.

Tuesday: Cloudy, 10-20 cm of new snow, light to moderate southwest winds, alpine high temperatures near-2 C with freezing level around 1100 m.

Avalanche Summary

A couple small avalanches, both human and explosive-triggered, have been reported in the new snow. These avalanches released on leeward aspects (north to northwest facing slopes) near tree line.

Reports from earlier in the week captured widespread large to very large (size 2-3) natural persistent slab avalanches, along with numerous explosive-triggered size 2-3 avalanches, targeted in the Whistler area. Many more size 2-3 avalanches were triggered by explosives and by skiers on Saturday and Sunday.

Of the avalanches mentioned above, many either failed on the mid-November weak layer or stepped down to it, even scouring the lower snowpack away to reveal ground. Some of the avalanches were remotely triggered. See here for some photos of one of them.

Human-triggering large avalanches remains a real possibility at higher elevations. Very cautious route-finding and conservative decision-making is currently required for safe travel at higher elevations.

Snowpack Summary

15-25 cm of new snow from the last 48 hours fell on a mix of crusts or old snow surfaces that are not likely to bond well, and moderate to strong southwest winds have drifted the new snow into reactive slabs on leeward features.

Below this recent snow, the upper snowpack consists of around 70 to 120 cm from last weekend's storm, which overlies a variable weak layer of surface hoar and a crust as well as a deeper (100-200 cm) weak layer of sugary faceted grains and a crust buried in mid-November. Both of these persistent weak layers produced many large and destructive avalanches during and in the days after the storm, often with light triggers and even remote triggers. Avalanche activity on these layers has been on a downward trend, but our fundamentally unstable snowpack structure remains a serious concern in the region. Snowpack tests continue to produce sudden results on these layers.

Managing your risk through conservative terrain choices along with selective avoidance of high-consequence avalanche terrain is strongly advised until the snowpack gains strength. It is atypical for the region and is expected to persist for some time.

Terrain and Travel

  • In times of uncertainty conservative terrain choices are our best defense.
  • Persistent slabs have potential to pull back to lower angle terrain.
  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • If triggered, wind slabs avalanches may step down to deeper layers resulting in larger 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.

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.

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.