Avalanche Forecast

Archived

Mar 31st, 2024–Apr 1st, 2024

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches possible, human triggered probable.

Below Treeline

Natural avalanches unlikely, human triggered possible.

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches possible, human triggered probable.

Below Treeline

Natural avalanches unlikely, human triggered possible.

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches possible, human triggered probable.

Below Treeline

Natural avalanches unlikely, human triggered possible.

Regions

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

Rising freezing levels and solar radiation will increase the hazard in the afternoon on Monday. Expect to find changing conditions as you change aspect and elevation.

Confidence

Moderate

Avalanche Summary

No new avalanche activity reported on Sunday.

Snowpack Summary

15-30cm of snow sits over the March 19th crust which is present everywhere except North aspects above 1900m. Widespread wind effect in the alpine. The Feb 3rd crust interface is down 30-90cm. Basal depth hoar and facets make up the bottom of the snowpack. HS ranges from 50 to 150cm.

Weather Summary

Mountain Weather Forecast is available @ Avalanche Canada https://avalanche.ca/weather/forecast

Monday

Cloudy with sunny periods and isolated flurries. Wind W: 15-30 km/h. Freezing level: 2100m.

Tuesday

Mainly cloudy with scattered flurries (4 cm). Wind SW: 25 km/h gusting 70 km/h. Freezing level: 2500m.

Wednesday

Flurries (10 cm). Wind SW: 15 km/h gusting to 45 km/h. Freezing level: 2200m.

Terrain and Travel Advice

Conditions may have improved, but be mindful that deep instabilities are still present.
If triggered, wind slabs avalanches may step down to deeper layers resulting in larger avalanches.
Be carefull around freshly wind loaded features.
Be alert to conditions that change with elevation and sun exposure.

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.

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.

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.