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Avalanche Forecast

Archived

Mar 24th, 2022–Mar 25th, 2022

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, human triggered possible.
Below Treeline
Natural avalanches unlikely.

Regions

South Coast Inland.

Travel conditions may be challenging with the latest surface crust. If you head to higher elevations, watch for pockets of wind loaded snow. 

Confidence

High - The snowpack structure is generally well understood.

Weather Forecast

THURSDAY NIGHT: Increasing cloud. Light to moderate southerly winds. Freezing levels drop to 1000 m.

FRIDAY: Mostly cloudy with isolated flurries. Moderate southerly winds and freezing levels around 1500 m.

SATURDAY: Mostly cloudy. Up to 3 cm overnight, and 5 cm possible over the day, freezing levels 1500-2000 m. Moderate to strong southerly winds. 

SUNDAY: Mostly cloudy, up to 10 cm of snow. Freezing levels 1500-2000 m. Moderate southwest winds. 

Avalanche Summary

On Wednesday a natural cycle of wet avalanche activity was reported up to size 2.5 around the Coquihalla highway. Activity mainly occurred from steep terrain features, affected by the warmer temperatures, rain and sun. 

A naturally triggered size 2 slab avalanche was reported on a northwest facing slope at treeline, involving the buried weak layers from mid March. 

Snowpack Summary

As temperatures drop, a melt freeze crust on all aspects will extend to treeline, and may extend into the alpine in some terrain. Expect moist snow at low elevations below the freezing line, and on south facing slopes as the sun comes out. Dry snow can be found at alpine elevations, likely redistributed by strong southerly winds into wind loaded features on north/east facing slopes. 

A melt-freeze crust from mid March exists down 30 to 60 cm on all aspects below 1500 m. The mid and lower snowpack is thought to be well settled and strong at this time. 

Terrain and Travel

  • Minimize exposure to sun-exposed slopes when the solar radiation is strong.
  • When a thick, melt-freeze surface crust is present, avalanche activity is unlikely.
  • Avoid freshly wind loaded features, especially near ridge crests, roll-overs and in steep terrain.
  • Pay attention to cornices and give them a wide berth when traveling on or below ridges.

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.