Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Apr 13th, 2017–Apr 14th, 2017

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.

Regions

South Coast Inland.

You may encounter unstable snow behind ridgelines or summits, especially in wind effected areas.

Confidence

Moderate - Due to the number of field observations

Weather Forecast

Friday: Flurries. Freezing level around 1700 m. Winds 10-20 km/h from the southwest. Saturday: Mostly dry with some sun appearing in the afternoon. Freezing level around 1700 m. Winds mostly calm. Sunday: Dry, with sunshine, especially in the morning. Freezing level rising to 1900 m. Light southeasterly winds.

Avalanche Summary

On Tuesday, a size 1.5 cornice triggered avalanche was reported on a north aspect at 2200 m in the Duffey Lake area.

Snowpack Summary

Relatively light amounts of recent snow have created wind slabs in the immediate lee of exposed terrain features at treeline and above. On sun solar aspects and at lower elevations, numerous crusts exist in the upper snowpack which are generally well bonded. Cornices are large and remain a concern: Saturday's fatal accident near Lions Bay illustrates the danger of them breaking off, and the large avalanches they can trigger.

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.

Cornices

Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.