Snow, rain and strong winds combined with buried weak layers make the perfect recipe for avalanches. Check out the new Forecasters Blog @ avalanche.ca.
Weather Forecast
Is spring the new winter? Waves of precipitation will continue overnight Friday and into Saturday. Amounts 10-15 mm on Saturday are expected, ridgetop winds moderate from the SW and freezing levels 1900 m. A dry day with a mix of sun and cloud is forecast on Sunday. Monday will see somewhat cooler temperatures with freezing levels near 1500 m and light precipitation 3-7 mm. The pattern looks to continue as a series of fronts and ridges move across the province throughout next week.
Avalanche Summary
Thursday was a fairly stormy day and observations are minimal but I suspect natural avalanche activity occurred. On Wednesday, natural and skier triggered slab avalanches were reported up to size 2. Both avalanches were reportedly over steeper convex terrain features on northerly aspects above 2100 m. Widespread natural avalanche activity is expected through the weekend with new snow, rain and strong SW winds.
Snowpack Summary
At higher elevations, new storm snow 20-30 cm sits over a plethora of surfaces including moist snow, crusts, wind affected surfaces, and/or old wind slabs. This gives us anywhere from 40-80 cm over the mid-February persistent weak interface. This interface has recently been very reactive and I don't suspect that to change during this stormy period. Strong winds have redistributed new snow into wind slabs on leeward terrain features. Lower elevations up to treeline are sporting spring-like, melt-freeze conditions. The late-January crust/surface hoar layer (over 1m deep) and the mid-January surface hoar (around 1.5m deep) have been dormant for several weeks.
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.
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.
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.