Avalanche Forecast

Archived

Apr 25th, 2025–Apr 26th, 2025

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Below Threshold.

Below Treeline

Below Threshold.

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Below Threshold.

Below Treeline

Below Threshold.

Alpine

Natural avalanches unlikely, human triggered possible.

Treeline

Below Threshold.

Below Treeline

Below Threshold.

Regions

Jasper, Brazeau, Churchill, Cirrus-Wilson, Fryatt, Icefields, Maligne, Marmot, Miette Lake, Pyramid.

A weekend warming trend and poor overnight refreeze will destabilize the snowpack. Watch for overhead hazards and avoid terrain capable of producing large avalanches.

Watch for isolated wind slabs in the high alpine and thin to thick snowpack areas where triggering the deep persistent slab is more likely.

Confidence

Moderate

Avalanche Summary

No recent observation.

Snowpack Summary

In sheltered northerly slopes above 2600m, 5-20 cm of soft snow exists. Isolated wind slabs exist on wind exposed lee slopes in the alpine.

The upper snowpack at treeline and below is a series of crusts. The lower snowpack is dry, faceted, and weak.

High north aspects offer the best spring riding conditions, though the snowpack remains susceptible to triggering deeper, unstable layers.

Weather Summary

Freezing levels will only drop to 2600 m Friday evening. On Saturday, freezing levels are expected to remain at or above this elevation, with a chance of afternoon thunderstorms. This warming trend will continue through the weekend, with rain or snow possible at higher elevations.

Terrain and Travel Advice

Back off slopes as the surface becomes moist or wet with rising temperatures.
Loose avalanches may step down to deeper layers, resulting in larger avalanches.
Avoid shallow, rocky areas where the snowpack transitions from thick to thin.
Back off if you encounter whumpfing, hollow sounds, or shooting cracks.

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.

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.

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.