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Avalanche Forecast

Archived

Mar 4th, 2021–Mar 5th, 2021

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 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

South Coast Inland.

Heavy snowfall and strong winds are expected to impact areas north in the region. Dial back terrain choices where you find 20 cm of new snow. Sustained warming remains a concern in the south of the region.

Confidence

Moderate - Recent weather patterns have resulted in a high degree of snowpack variability within the region.

Weather Forecast

Heavy snowfall and strong winds are expected to impact the north of the region

Thursday night: 

North: Overcast, 5-10 cm of snow, moderate to strong south winds, freezing level dropping to 1400 m. 

South: Mostly cloudy, a trace of snow, moderate south winds, freezing level dropping to 1700 m.

Friday: 

North: Overcast, 10-15 cm of snow, moderate to strong south winds, freezing level rising to 1500 m then falling to 500 m. 

South: Mostly cloudy, a trace of snow, moderate south winds, freezing level rising to 2000 m then falling to 500 m. 

Saturday: Mostly cloudy, isolated flurries with trace accumulations, light southwest winds, freezing level near 1300 m.

Sunday: Mostly cloudy, isolated flurries with trace accumulations, light southwest winds, freezing level near 1200 m.

Avalanche Summary

In the north of the region, natural and human-triggered avalanches from new snow and wind are likely on Friday. 

There are still concerns about the reactivity of persistent weak layers in these areas. Over the past week, observers near Duffey Lake reported a large (size 2.5) avalanche on a north aspect at 1750 m that was thought to have released 1 m deep on a persistent weak layer. On Sunday, a size 1.5 skier accidental was reported on a northwest aspect in the alpine, also near Duffey Lake. The slab is thought to have failed on a thin layer of facets, sandwiched between two wind-stiffened layers. 

In the south of the region, an observer submitted this MIN report of large wet avalanche activity near Manning Park on Tuesday. In the Coquihalla area, several natural glide slab avalanches size 2-2.5 have been observed. Glide slabs are notoriously difficult to forecast but with the sustained warming, we may see continued activity. Glide slabs are most likely in areas of smooth ground cover such as rock slabs at lower elevations experiencing prolonged warm temperatures with limited overnight refreeze. These avalanches will be large, involving the full depth of the snowpack. Carefully consider your access/egress routes where they cross under large paths. 

Snowpack Summary

The focus for avalanche hazard in the region shifts to the north with an incoming storm. Above freezing temperatures remain a concern in the south of the region on Friday, but danger ratings are a full step lower (Considerable, Considerable, Moderate). 

In the north of the region, an incoming storm is forecast to bring 15-25 cm of snow by midday on Friday. Strong south winds will contribute to rapid slab formation, making natural avalanches likely. The combination of wind and snow has the potential to weaken cornices, which can act as triggers on slopes below. 

The rapid load from new snow and wind has the potential to wake up buried weak layers. A layer of facets from mid-February has shown reactivity on north aspects near treeline and is primarily a concern where it separates wind-stiffened snow above and below. A deeper persistent weak layer buried in late January composed of a crust, facets or surface hoar also has the potential to re-awaken with large triggers, such as an avalanche in motion, cornice fall, or intense loading from snow/ wind. The lower snowpack is well settled and strong in most areas.

In the south of the region, the snowpack is generally well consolidated with no concerns of buried weak layers.

Terrain and Travel

  • Watch for fresh storm slabs building throughout the day.
  • Dial back your terrain choices if you are seeing more than 20 cm of new snow.
  • Use conservative route selection. Choose simple, low-angle, well-supported terrain with no overhead hazard.
  • Storm slabs in motion may step down to deeper layers resulting in large avalanches.
  • Avoid steep slopes when air temperatures are warm, or solar radiation is strong.

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.

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.