Regions
South Coast Inland.
Cornices and surface snow could become weak when hit by direct sunlight.
Confidence
Moderate - Due to the number and quality of field observations
Weather Forecast
TUESDAY: Clouds clearing in the morning and then sunny in the afternoon, light west wind, freezing level rising to around 1000 m.WEDNESDAY: Sunny, light to moderate southwest wind, freezing level rising to around 1300 m.THURSDAY: Flurries increasing throughout the day with up to 5 cm of snow by the afternoon, moderate southwest wind, freezing level rising to around 1200 m.
Avalanche Summary
On Sunday, a large natural avalanche (size 2) was observed on a sparsely treed north-facing slope at 2000 m in the northern part of the region.On Saturday, one natural size 2 slab was observed on a south aspect at 1900 m in the Duffey area and another smaller slab was reported on a steep wind-loaded feature in the Coquihalla area. Wet loose avalanches were observed in steep south-facing terrain throughout the region.On Friday, wind slabs were sensitive to skier triggering to size 2 on north and northeast facing slopes around 2000 m. These slabs were 10 to 25 m wide with crowns averaging 40 cm in depth.
Snowpack Summary
A thin sun crust has formed on solar aspects and the surface is wind affected in most exposed terrain. Southern parts of the region, such as the Coquihalla, received up to 100 cm of snow last week while northern regions received closer to 40 cm.The mid-February weak layers are now 80 to 120 cm deep in the southern part of the region and about 40 cm deep in northern parts of the region. These interfaces consists of wind hardened snow, facets, a sun crust on solar aspects, and surface hoar that is present at and below treeline. Some of these layers have been reactive in snowpack tests, but no recent avalanche activity has been reported on these layers. The mid and lower snowpack are well settled and strong.Variable winds in the past month have created cornices on many alpine ridgelines. They will become touchier as they grow in size, as temperatures rise, and as the strong late-winter sun shines down upon them on clear days.
Problems
Wind Slabs
Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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.