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Avalanche Forecast

Archived

Mar 4th, 2021–Mar 5th, 2021

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

Regions

Kootenay Boundary.

Sustained warm temperatures will keep avalanche danger elevated on Friday, particularly on slopes getting direct sun. Be prepared to back off steep slopes when the snow becomes wet or slushy. 

Confidence

Moderate - Uncertainty is due to how the snowpack will react to the forecast weather.

Weather Forecast

Thursday night: Mostly clear, moderate southwest wind, freezing level remaining above 2100 m.

Friday: Clear with clouds moving in for the afternoon, moderate south wind, freezing level remaining above 2100 m.

Saturday: Mostly cloudy, 5-10 cm of snow, moderate southwest wind, freezing level near 1500 m.

Sunday: Mostly cloudy, 5-10 cm of snow, moderate southwest wind, freezing level near 1300 m.

Avalanche Summary

Numerous large (size 2) wet loose avalanches released naturally on south-facing aspects between 1700-2000 m over the past few days of sunny, warm weather.

Over the weekend, there were a few natural and skier triggered wind slabs size 1.5. On Saturday, large explosives produced very large (size 2-3) results at Kootenay Pass. In thin snowpack areas on solar aspects, a few of these large avalanches are suspected to have stepped down to the January layer described in the snowpack summary.

Snowpack Summary

Elevated freezing levels and sun will continue melting, and potentially destabilizing, snow surfaces on Friday. Watch for pinwheels and roller balls, as they are a clear indication of wet loose avalanche activity. You can avoid them by staying off steep slopes when the snow becomes wet or slushy.  

At upper elevations, snow is wind-pressed in most exposed areas, and a melt freeze crust is forming on sunny slopes. In shaded, sheltered areas, 15-30 cm of well-settled snow may sit over a layer of small surface hoar crystals buried Feb 25th. A more prominent persistent weak layer from late January is buried 80-150 cm deep and is composed of a combination of surface hoar, crusts, and facets. The problem seems to be most pronounced in thin snowpack areas on solar aspects. The current impulse of warming will likely be the final test on these layers, as there is some uncertainty about whether they will become reactive again under these conditions.

As described in this MIN report, shallow snowpack areas in the east of the region may harbor a faceted basal snowpack. This structure can typically be managed by avoiding shallow rocky areas where the snowpack transitions from thick to thin. This is another layer that could be susceptible to shock from the warm temperatures this week. Extra caution should be exercised in these shallow snowpack areas.

Terrain and Travel

  • Back off slopes as the surface becomes moist or wet with rising temperatures.
  • A moist or wet snow surface, pinwheeling and natural avalanches are all indicators of a weakening snowpack.
  • If triggered loose wet avalanches may step down to deeper layers resulting in larger avalanches.
  • Avoid shallow, rocky areas where the snowpack transitions from thick to thin.

Problems

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.

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.