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Avalanche Forecast

Archived

Jan 14th, 2019–Jan 15th, 2019

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

Regions

South Coast.

The mid-winter summer break continues. A warm snowpack can weaken quickly, use caution around cornices and steep slopes until temperatures drop.

Confidence

Moderate - Freezing levels are uncertain

Weather Forecast

MONDAY NIGHT: Clear. Freezing level dropping below 500 m. Alpine high low near +5. Light winds.TUESDAY: Sunny and warm. Freezing level near 2200 m. Alpine high near +4. Light winds.WEDNESDAY: Mix of sun and cloud. Freezing level near 1500 m. Alpine high near +5. Light to moderate east-southeast winds.THURSDAY: Rain, 25 mm. Freezing level 1700 m. Alpine high near +6. Moderate east wind gusting strong.More details can be found in the Mountain Weather Forecast.

Avalanche Summary

On Friday, loose wet avalanches released naturally below 1200 m. Skiers were able to trigger loose wet avalanches which ran on an ice layer down 15-20 cm. Size 2 wet slabs were also observed in the Sky Pilot area. These are thought to have occurred on Thursday or Friday. We appreciate any observations shared on the Mountain Information Network here.

Snowpack Summary

Warm temperatures have created moist surface snow, which has refrozen into crusts at low elevations and on sunny aspects. In the north of the region, you may find wind-affected snow or dry snow (on shady aspects) at upper elevations. Lingering cornices may fail with warming. A solid surface crust exists below about 1700 m.

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.

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.