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Avalanche Forecast

Archived

Mar 27th, 2021–Mar 28th, 2021

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

Regions

North Columbia.

Avalanche danger will increase through the day as new snow and wind form touchy storm slabs. Stick to simple, wind-sheltered terrain.

Confidence

High - We are confident the likelihood of avalanche will increase with the arrival of the forecast weather.

Weather Forecast

Saturday night: 5-15 cm new snow, 40-50 km/h southwest wind. Freezing level 1500 m. Alpine temperature -5.

Sunday: 10-20 cm new snow. 50-70 km/h southwest wind. Freezing level up to 1500 m. Alpine temperature -5.

Monday: Flurries. 30 km/h northwest wind. Freezing level drops to valley bottom. Alpine temperature -13

Tuesday: Mix of sun and cloud. 20 km/h northwest wind. Freezing level 1400 m. Alpine temperature -8.

Avalanche Summary

Recent avalanche activity has primarily been small (size 1-1.5) wind slab and dry loose avalanches in the top 20 cm of snow. A few larger slab 2 avalanches have been observed in steep slide paths in Glacier NP over the past few days. One notable size 3 slab avalanche was observed northeast of Revelstoke on Wednesday. The avalanche failed on the ground on a south aspect at 1600 m. While an isolated event, it is a good reminder to watch for slopes warming up in the springtime heat.

Snowpack Summary

With 5-20 cm forecast per 12 hour period, by Sunday afternoon you could see 20 to 40 cm of fresh snow. Accompanied by strong wind, this new snow will likely form touchy slabs. 

50-100 cm now sits above an interface that formed during the mid-March dry spell, which consists of a widespread crust (except on north-facing slopes above 1800 m). Overall the snow seems to be bonding well to this interface, although there have been some isolated human triggered avalanches running on the crust layer over the past few days.

Lower elevations have undergone daily melt-freeze cycles, with moist or crusty surfaces likely found up to at least 1600 m.

Terrain and Travel

  • Watch for fresh storm slabs building throughout the day.
  • As the storm slab problem gets trickier, the easy solution is to choose more conservative terrain.
  • Choose low-angled, sheltered terrain where new snow hasn't been wind-affected.

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.