Avalanche Forecast

Archived

Apr 15th, 2023–Apr 16th, 2023

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches unlikely, human triggered possible.

Below Treeline

Below Threshold.

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches possible, human triggered probable.

Below Treeline

Below Threshold.

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches unlikely, human triggered possible.

Below Treeline

Below Threshold.

Regions

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

Freezing levels will rise on Sunday, with 5-10 cm of new snow and strong SW winds expected Sunday night and into Monday. Hazard will increase later on Sunday and into Monday as the storm arrives with increased potential for triggering the deep persistent weak layers.

Confidence

Moderate

Avalanche Summary

The recent avalanche cycle produced large natural avalanches in most of the forecast area, with lots of failures on storm snow interfaces and many step downs to the various deeper persistent weak layers in the snowpack. Natural avalanche activity has slowed in the last two days but we are still able to trigger large avalanches with explosives.

Snowpack Summary

Recent storm snow has settled to 20-30 cm above 2300 m. The storm snow sits over buried sun crusts that are present to ridge crests, and faceted layers on shady aspects. Multiple buried crusts are present in the top 50-70 cm on solar aspects. The basal depth hoar is present at the bottom of the snowpack and remains facetted and weak. Low elevations have a temperature crust on all aspects.

Weather Summary

On Sunday, winds will gradually increase into the moderate to strong range out of the SW. Freezing levels will start to rise, reaching 2100-2300 m late in the day. Precip will start in the late afternoon with 5-10 cm expected overnight and into Monday and rain is possible at valley bottom elevations.

Terrain and Travel Advice

Keep in mind that human triggering potential persists as natural avalanching tapers off.
If triggered, storm slabs in-motion may step down to deeper layers and result in very large avalanches.
Use extra caution around cornices: they are large, fragile, and can trigger slabs on slopes below.

Problems

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.

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.