Avalanche Forecast

Archived

Apr 22nd, 2025–Apr 25th, 2025

Alpine

Natural avalanches unlikely, human triggered possible.

Treeline

Below Threshold.

Below Treeline

Below Threshold.

Alpine

Natural avalanches unlikely, human triggered possible.

Treeline

Below Threshold.

Below Treeline

Below Threshold.

Alpine

Natural avalanches unlikely, human triggered possible.

Treeline

Below Threshold.

Below Treeline

Below Threshold.

Regions

Kananaskis, Bow Valley, Highwood Pass, North 40, Spray - KLakes.

Spring conditions exist in most locations. North aspects may still hold the persistent problem, be cautious and inspect. This is the time of year to start early and finish early. Watch for warming and direct solar input when travelling through terrain. Check out Avalanche Canada's blog on Spring Conditions for some good tips.

Confidence

Moderate

Avalanche Summary

No recent activity observed or reported.

Snowpack Summary

The snowpack is steadily transitioning to a Spring snowpack.

On north aspects in the Alpine, dry snow can still be found, and weaknesses in the lower snowpack could still be triggered, as these areas have not completely morphed into a Spring snowpack. Otherwise all other aspects and elevations consist of multiple layers of crusts and/or a well settled snowpack. These crusts will break down through the day depending on air temperatures and solar radiation. There are still many areas with basal facets/depth hoar that could awaken if the snowpack gets warm enough.

Timing is everything. As surface crusts break down during the day the avalanche hazard will begin to increase. Start early and finish early.

Weather Summary

Wednesday should be a mix of sun and cloud with light winds and no precipitation. Thursday and Friday will be warmer. Freezing levels will steadily increase each day:

Wed - 2200m

Thurs - 2600m

Friday 2800m

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

Even brief periods of direct sun could produce natural avalanches.
Travel early on sun-exposed slopes before cornices weaken with daytime warming.
Avoid steep, sun-exposed slopes when the air temperature is warm or when solar radiation is strong.
Be careful with wind-loaded pockets, especially near ridge crests and rollovers.

Problems

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.

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.