Spring Conditions. Looks like a typical spring day with a mix of conditions. The sun can be very strong at this time of year; conditions may change rapidly if the sun comes out.
Weather Forecast
Mostly clear overnight with moderate southwest winds and freezing levels down to 1000 metres. Mix of sun and cloud on Friday with scattered convective flurries and daytime freezing levels at 2200 metres. A strong ridge develops on Saturday bringing clear skies, moderate southerly winds and freezing levels up to at least 2500 metres. The ridge gets stronger on Sunday, temperatures and freezing levels sky-rocket to at least 3000 metres.
Avalanche Summary
One small size 1.0 skier controlled wind slab was reported on Wednesday from a steep north aspect in the high alpine. Most commercial operations in the region have closed for the season, and data has become sparse.
Snowpack Summary
The snow surface is currently going through a typical spring melt-freeze cycle on all aspects and at all elevations, except possibly high true-north slopes which could be holding onto cold snow. The strength (thickness) of the surface crust and how quickly it breaks down during the day are important factors to focus on. Watch for new snow releasing as loose wet avalanches when the sun comes out. Thin new wind slabs may be easy to trigger when they are exposed to strong solar radiation. Watch for very warm temperatures developing this weekend.
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.