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Avalanche Forecast

Archived

Mar 31st, 2024–Apr 1st, 2024

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

Regions

Northwest Coastal, Boundary, Kitimat, Rupert, Stewart, Ningunsaw, Ningunsaw, Ningunsaw.

As flurries accumulate, check for wind-loaded deposits around ridges and lee features.

Confidence

High

Avalanche Summary

There have been no new avalanches reported in the last couple days.

A week ago (Sat Mar 23), three very large (size 3) persistent slab avalanches were reported, occurring on southerly alpine slopes and likely triggered by warming.

Snowpack Summary

Dry snow still exists on north-facing slopes at upper elevations. A thin layer of surface hoar may be growing in sheltered terrain. In most areas, a thick widespread crust caps the snowpack. At lower elevations and on steep sunny slopes, the crust may soften with warming during the day or the snowpack may become isothermal.

Various weak layers, including crusts, facets, and/or surface hoar exist approximately 40 to 80 cm deep. An additional crust and facet layer may be found 100 to 150+ cm below the surface. This problem is trending into dormancy, however, lingering concern remains for human-triggering on these persistent weak layers.

Weather Summary

Sunday Night

Mostly clear with incoming clouds. West-southwest ridgetop wind 30 to 60 km/h. Treeline temperature low -10 °C. Freezing level valley bottom.

Monday

Flurries, 5 to 15 cm. South ridgetop wind 20 to 40 km/h. Treeline temperature high -4 °C. Freezing level valley bottom.

Tuesday

Snow and flurries, 15 to 25 cm. Southwest ridgetop wind gusting to 60 km/h. Treeline temperature -4 °C. Freezing level near 800 m.

Wednesday

Cloudy with isolated flurries. Light and variable ridgetop wind. Treeline temperature -5 °C. Freezing level valley bottom.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Avoid freshly wind loaded features, especially near ridge crests, roll-overs and in steep terrain.
  • Wind slabs may be poorly bonded to the underlying crust.
  • Avoid thin areas like rock outcroppings where you're most likely to trigger avalanches failing on deep weak layers.
  • When a thick, melt-freeze surface crust is present, avalanche activity is unlikely.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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.