I expect a natural avalanche cycle to occur in the Coquihalla backcountry areas on Tuesday as the wind increases in the afternoon. Avalanche danger for the alpine along the Duffey is more like CONSIDERABLE.
Confidence
Poor - Due to variable snowpack conditions
Weather Forecast
Synopsis: A punchy Pacific frontal system will bring heavy precipitation Tuesday night and Wednesday.Tuesday: Day starting clear, but clouding over then moderate snowfall starting in the afternoon. Southerly winds 40 km/h.Tuesday Night: 10-20 cm overnight. Freezing level around 1200 m. Southwest winds increasing to 60 km/h at ridgetop.Wednesday: 10-20 cm new snow. Freezing level around 1500 m. Southwest winds 60 km/h.Thursday: 5-15 cm new snow. Freezing level 800 m. Gusty westerly winds becoming northwest later on.
Avalanche Summary
On Sunday, slab avalanches were easily human-triggered up to size 2 in the Coquihalla on south aspects with 40-60 cm storm snow failing on a crust. On Friday, a size 2.5 natural loose wet avalanche was reported from the Coquihalla. Along the Duffey, small skier-triggered avalanches could be triggered on north aspect slopes at treeline, with crowns of 30 cm in the recent storm snow.
Snowpack Summary
Heavy snowfall has continued in the Coquihalla region, with recent storm totals over the last four days of 80 cm. During the same period, around 20 cm fell along the Duffey and around 30 cm in Manning Park. This new snow sits on a crust along the Duffey at elevations below 1900 m. In the Coquihalla region, this crust was not reported to have formed due to the insulating effect of the new snow. Instead, the new snow here sits on wet snow from the previous storm. For all areas, expect extensive wind slabs and cornices in the alpine. A deeper weak layer comprising surface hoar and/or a crust is buried around 70 cm on the Duffey/in Manning Park and more like a metre on the Coquihalla. Natural avalanche activity has subsided on this layer. However, I wouldn't discount the possibility of an avalanche stepping down to this layer, especially in steep alpine terrain. Lower snowpack layers are strong and well settled, although the snowpack may still be susceptible to glide activity (involving the whole snowpack) at lower elevations where it rests on steep, smooth surfaces.
Problems
Storm Slabs
Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.