Weather Forecast
Clear skies, light winds, and warm sunny days are expected for the forecast period. Temperatures are expected to drop below zero overnight providing a good re-freeze of the surface snow. Freezing levels during the day are expected to rise to about 1400 metres.
Avalanche Summary
Widespread wet loose and surface slab activity on solar aspects up to size 2.5 in the Coquihalla area. No new reports from the Duffey lake area, on Friday moist slab releases up to size 3.5 were observed running full path on southerly aspects due to solar warming and warm overnight temperatures in the alpine.
Snowpack Summary
Thin sun crusts are developing on steep solar aspects. The recent storm snow continues to settle and bond in the Duffey Lake area due to the warm temperatures and light winds. Recent cornice growth may be easy to trigger with light loads or from solar radiation. The Coquihalla area is also experiencing warm temperatures and light winds. The storm slab in the Coquihalla is about a metre deep and continues to settle and bond with warm temperatures. Concern for steep solar aspects in the alpine with shallow or variable snowpack depths.
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.