Avalanche conditions are very dangerous at this time.
Weather Forecast
Friday night: 5-10 cm new snow expected to fall, with freezing levels around 1000 m and SW winds gusting 60-80 km/h. Saturday: Light precipitation, ramping up in the afternoon, with 10-15 cm new snow anticipated by the end of the day. Moderate southwest winds are expected with freezing levels around 1000 m. Sunday: An additional 15-25 cm new snow is expected by the end of the day. Winds strong southwesterly. Freezing levels staying around 1000m. Monday: Another, more intense storm system arrives, bringing 40-50 cm new snow, temperatures cool enough for snow at most elevations and high winds.
Avalanche Summary
There have been at least two close calls involving snowbobile-triggered avalanches in the region over the last couple of days, one of which was triggered from 200m away from below. A size 2 natural avalanche was reported from Garibaldi Park at 1800m on a N aspect on Friday. There was an avalanche fatality in the Brandywine area on Tuesday. So far we know that a single snowmobiler was buried and perished in a Size 3 avalanche. The avalanche occurred on an east aspect at approximately 1700m, the slab was estimated to be 1.5-2.0m thick and 400m wide and suspected to have stepped-down to the mid-February persistent weakness. W. More reports of last weekend's widespread large natural avalanche cycle are coming in with observations of Size 4.5 avalanches. Some of the larger slabs propagated 2-3Km along ridgelines and stepped down to the mid-February persistent weakness, and there's no reason why similar avalanches can't happen with this next round of loading.
Snowpack Summary
New snow accompanied with strong southwest winds are setting up new storm slabs and wind slabs overlying a variable previous snow surface comprising crusts, moist snow and old wind slabs. Previous storm snow amounts were in the region of 50+ cm and this snow bonded poorly to the older surfaces below. The instabilities associated with both these storm slabs as well as deeper weak layers buried within the snowpack have given us a situation where avalanches could initiate in the upper storm snow and easily propagate to lower weaknesses in the snowpack. This dramatically increases the potential size of avalanche occurrences, which is pushing up into the size 3-4 category. There is also the possibility for avalanches to be remote-triggered, triggered mid-slope, and/or propagate into low-angled terrain.
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.
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.
Persistent Slabs
Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.