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.
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.
A warm snowpack can weaken quickly, use caution around cornices and steep slopes until temperatures drop.
Confidence
Moderate - Intensity of incoming weather systems is uncertain on Thursday
Weather Forecast
TUESDAY NIGHT: Cloudy with clear periods. Freezing level dropping below 1600 m. Alpine low +2. Light southeast winds.WEDNESDAY: Mix of sun and cloud. Freezing level near 1900 m. Alpine high near +3. Light to moderate east-southeast winds.THURSDAY: Showers, 10 mm. Freezing level near 1500 m. Alpine high near +3. Moderate south-southwest wind gusting strong.FRIDAY: Periods of rain, 15-20 mm. Freezing level rising to 1700 m. Alpine high near +3. Moderate southwest winds.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 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
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.
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.