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Avalanche Forecast

Archived

Mar 29th, 2022–Mar 30th, 2022

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

Regions

Kootenay Boundary.

Overnight refreezing of the snowpack may be poor. If you find wet and heavy surface snow in the morning minimize your exposure to avalanche terrain as wet avalanches are more likely. 

Watch for changing conditions throughout the day. 

Confidence

Moderate - Uncertainty is due to difficult to forecast freezing levels.

Weather Forecast

TUESDAY NIGHT: Mostly clear skies with light southwest winds. Freezing levels peak at 2500 m overnight, and cools into the morning. 

WEDNESDAY: Mix of sun and cloud with moderate southwest winds (strong gusts possible). Light snowfall with 5-10 cm possible. Snowfall is likely to be convective flurries, and accumulations favour Kootenay Pass. Freezing levels around 1800 m, alpine high +4. 

THURSDAY: A mix of sun and cloud, light to moderate westerly winds. Isolated flurries possible. Freezing levels peak at 1500 m, alpine highs of +1.

FRIDAY: A mix of sun and cloud with light southwest winds. Freezing levels reach 1800 m. Alpine highs of +4. 

Avalanche Summary

On Monday, several loose wet avalanches were reported to size 2, including a cornice fall triggering the slope below. 

Wet avalanche activity is expected to continue during this warm weather pattern. 

Snowpack Summary

The upper snowpack is going through a daily melt-freeze cycle. A crust exists on all aspects to around 2500 m. Warm temperatures and sun are softening or breaking down the crust during the day and creating moist snow. At very low elevations, the snowpack may be wet and isothermal, depending on overnight freezing levels. 

At 40 to 70 cm below the snow surface, a sun crust exists on solar aspects, and weak surface hoar crystals sit on shaded aspects. This layer was buried in early March and produced surprising avalanches during the last storm and following warm days. Recent reports suggest this layer is now bonding well from the warm temperatures. 

The mid and lower snowpack are generally strong and well bonded.

Terrain and Travel

  • Be alert to conditions that change with elevation and sun exposure.
  • When a thick, melt-freeze surface crust is present, avalanche activity is unlikely.
  • As surface loses cohesion due to melting, loose wet avalanches become common in steeper terrain.
  • Minimize exposure to steep, sun exposed slopes, especially when the solar radiation is strong.

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.