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Avalanche Forecast

Archived

Mar 24th, 2023–Mar 25th, 2023

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

Regions

Vancouver Island, East Island, South Island, West Island.

Expect forecast new snow to take time to bond to a well established hard crust.

Carefully consider your terrain choices prior to committing to steep avalanche terrain, especially those with evidence of wind transport and loading.

Confidence

Moderate

Avalanche Summary

On Wednesday , field teams reported several loose wet avalanches on south aspect terrain. Explosive avalanche control utilizing a large explosive on a steep north aspect incised rocky gulley feature produced a large (size 2.5) slab avalanche. This avalanche ran on an old melt freeze crust, was 100 cm deep at the crown and ran to the bottom of the run out.

Backcountry users will likely see evidence of a small wet loose avalanche cycle from recent rain and solar input below treeline.

If you head out in the backcountry, let us know what you are seeing by submitting a report to the Mountain Information Network.

Snowpack Summary

In terrain above 1600 m up to 10 cm of preserved and wind affected dry snow is likely to exist. An established melt freeze crust can be found at elevations 1600 m and below, expect the new forecast snowfall to take a little time to bond to this old surface. At all elevations the mid and lower snowpack has a number of old melt freeze crusts that are unreactive and overall presents as consolidated, well settled and strong.

Weather Summary

Friday Night

Cloudy with flurries, 5 to 10 cm of accumulation. Moderate north winds at ridge top. Treeline temperature -1°C. Freezing levels rise to 1000 m.

Saturday

Cloudy with flurries, 1 to 5 cm of accumulation. Moderate north winds at ridge top. Treeline temperature -1°C. Freezing levels rise to 1000 m.

Sunday

Cloudy with very light flurries a trace to 2 cm of accumulation. Moderate southeast winds at ridge top. Treeline temperature 0°C. Freezing levels rise to 1000 m.

Monday

Mostly clear. No new precipitation. Moderate southeast winds at ridge top. Treeline temperature 0°C. Freezing levels rise to 1200 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Closely monitor how the new snow is bonding to the crust.

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.

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.