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Avalanche Forecast

Archived

Dec 17th, 2021–Dec 18th, 2021

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

Regions

South Coast.

Heavy snowfall and strong wind are creating very dangerous avalanche conditions. Avoiding avalanche terrain will be critical to managing your risk on Saturday. Stick to simple, low-angle slopes with no overhead hazard. 

Confidence

Moderate - Forecast precipitation (either snow or rain) amounts are uncertain.

Weather Forecast

Heavy snowfall and extreme wind on Saturday

Friday night: Overcast, 10-30 cm of snow above 600 m, strong southwest winds, treeline temperatures rising from -5 C to -2 C, freezing level rising from 300 m to 600 m.

Saturday: Overcast, 30-50 cm of snow above 1000 m, strong southwest winds with extreme gusts, treeline temperatures rising to near +2 C in the afternoon, freezing level rising to 1000 m, with freezing levels near 1300 m closer to the coast.

Sunday: Mainly sunny, 5-15 cm of snow overnight above 600 m, light east winds, high treeline temperatures near -3 C, freezing level around 600 m.

Monday: Increasing cloudiness, no snow expected, light south winds, high treeline temperatures near -2 C, freezing level around 100 m. 

Avalanche Summary

Natural avalanches releasing in the new snow are likely on Saturday. These storm slab avalanches are expected to be large, widespread, and very sensitive to human-triggers.

In the neighbouring Sea-to-Sky region on Thursday, we received reports of two large (size 2-3) human-triggered avalanches that released on a persistent weak layer between 1700-1900 m on west and southwest aspects. Notably, these avalanches were remote-triggered while party members were traveling uphill. Several small sympathetic avalanches were also thought to have released during these events. We have concern that this problem may extend into the south coast region at upper elevations in the north of region, such as near Sky Pilot. It may be possible to trigger very large avalanches in isolated areas on Saturday.

Pinwheeling and isolated small (size 1) wet loose avalanches were reported during the strong afternoon sun on Thursday.

Snowpack Summary

An intense storm is taking aim at the region, bringing extreme southwest winds and 40-80 cm of new snow by Saturday afternoon. During the heaviest snowfall midday on Saturday, freezing levels are forecast to rise to 1000 m, creating denser snow over lighter snow and potentially forming a mid-storm crust layer. Freezing levels may reach 1300 m in areas closer to the coast. Extreme southwest wind will likely be a major contributor to the size, likelihood, and distribution of Saturday's storm slab problem. Even open steep slopes below treeline should be treated as suspect on Saturday.

The new snow is falling on a mix of previous snow surfaces, including harder, wind-packed surfaces, a melt-freeze crust that may have formed on steep south-facing slopes during Thursday's sunny skies, or cold soft snow in sheltered areas. 

Small facets (sugary snow) can be found down 120-200 cm near two crust layers that formed in early December. On Tuesday, observers near Ski Pilot reported whumphing that is likely associated with this interface (see this MIN report). It may be possible to human trigger this persistent slab in thinner snowpack areas near ridge tops, where the facets are more developed and where the crust layers are more accessible to the weight of a person or machine.

Below these crust layers, the snowpack is generally well-settled. Early season hazards such as rocks, stumps, and open creeks remain at lower elevations. 

Terrain and Travel

  • Avoid all avalanche terrain during periods of heavy loading from new snow and wind.
  • Use increased caution at all elevations. Storm snow is forming touchy slabs.
  • Avoid the runout zones of avalanche paths. Avalanches could run full path.
  • Be aware of the potential for large avalanches due to the presence of a persistent slab.
  • Remote triggering is a concern, avoid terrain where triggering slopes from below is possible

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.