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Avalanche Forecast

Archived

Mar 25th, 2025–Mar 26th, 2025

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

Regions

Banff Yoho Kootenay, Banff, East Side 93N, Kootenay, Lake Louise, LLSA, Sunshine, West Side 93N, Field.

Climbing freezing levels and rainfall are driving HIGH avalanche danger. Steer clear of avalanche terrain until the storm passes and conditions stabilize.

Confidence

Moderate

Avalanche Summary

Lake Louise patrol reported numerous size 1's triggered by explosives. Sunshine patrol reported knocking out a size 2.5 on a reloaded bed surface which reacted like a deep slab, down to rocks. A field team member near Simpson Pass reported hearing a large audible avalanche.

Snowpack Summary

15-20 cm of heavy moist snow (up to 2400m) has been blown into windslabs up to 40 cm deep in leeward areas. This adds to the dense slab, 50-100 cm thick, overlying weak facets in the mid to lower snowpack and is responsible for the recent large avalanches. This condition has been most sensitive in the Bow Summit area, but expect the likelihood of avalanches to increase at all elevations with the warming.

Weather Summary

Freezing levels are on the rise, with moderate precipitation expected to bring another 10 cm of snow by Wednesday morning. Rain is likely at lower elevations. Winds will be variable and somewhat unpredictable, potentially reaching strong speeds from the southwest. Taken together, these factors point toward an avalanche cycle.

Terrain and Travel Advice

  • Make conservative terrain choices and avoid overhead hazard.
  • Avoid shallow, rocky areas where the snowpack transitions from thick to thin.
  • Remote triggering is a big concern, be aware of the potential for wide propagations and large, destructive avalanches at all elevations.

Problems

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.

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.