Avalanche Forecast

Archived

Mar 7th, 2023–Mar 8th, 2023

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches unlikely, human triggered possible.

Below Treeline

Natural avalanches unlikely.

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches unlikely, human triggered possible.

Below Treeline

Natural avalanches unlikely.

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches unlikely, human triggered possible.

Below Treeline

Natural avalanches unlikely.

Regions

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

Although natural avalanche activity has slowed down, human triggering of variable wind slab and of our deep persistent problem remains possible.Thin to thick areas are the most likely trigger points.

Solar radiation should also be considered this week - especially mid day through mid afternoon on steep southerly aspects, and in terrain exposed to cornices.

Confidence

Moderate

Avalanche Summary

No significant avalanches observed on a patrol of Hwy 93 Monday.

A number of large avalanches up to size 3 were observed last week. Natural activity has tapered off but the snowpack has proven sensitive to small inputs of new snow, loading, temperature change, and potentially solar effect. The majority of last week's large avalanches initiated in the alpine but have the potential to run through all elevation bands.

Don't forget to post avalanche observations to the MIN.

Snowpack Summary

In sheltered areas the top 20 to 40cm is comprised of low density facetted crystals. There is extensive wind effect at tree line and above from previous SW winds.

This is sitting on top of a generally weak mid and lower snowpack. Facets and depth hoar linger at the base of the snowpack with the height of snow varying from 60 to 160cm.

Weather Summary

The surface ridge of high pressure will remain in place until Friday. Clear skies, variable light wind, and temperatures slightly below seasonal are expected. Freezing level forecast to remain at or near valley bottom. An upper low may bring some flurries Friday and Saturday.

Detailed weather forecasts from Avalanche Canada: https://avalanche.ca/weather/forecast

Terrain and Travel Advice

If triggered, wind slabs avalanches may step down to deeper layers resulting in larger avalanches.
Avoid shallow, rocky areas where the snowpack transitions from thick to thin.

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.

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.