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Avalanche Forecast

Archived

Mar 31st, 2022–Apr 1st, 2022

Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Little Yoho.

Look for fresh thin wind slabs in the alpine and avoid them. Although flurries and cloud is forecasted Friday, be mindful of any significant periods of sun and the warmth through the day. If the crusts break down, the hazard may rise to moderate.

Weather Forecast

Scattered flurries and partly cloudy skies are forecasted for Friday. Winds (SW) will taper through the day from 40-50 km/hr to 20-30 km/hr. Freezing levels on Friday may rise up to 2000 m and then drop to valley bottom Thursday and Friday night. For more details, click here.

Snowpack Summary

Isolated thin windslabs exist in the alpine and mostly noted on immediate lee of features. Surface melt-freeze crusts exist on all aspects up to approx. 2300m and higher on solar aspects. On high elevation north aspects dry snow exists. The mid-pack is well settled but has several persistent layers consisting of crusts and/or facets.

Avalanche Summary

In the alpine, a few 1.5 thin windslabs were ski cut/triggered in the region on Thursday. A fresh size 3 avalanche was observed on the main highway path on Mt. Stephen on Wednesday. This was likely serac triggered.

Confidence

Timing or intensity of solar radiation is uncertain

Problems

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.

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.