Warm temperatures and sunny skies forecast for the next few days will have a significant weakening effect on the snowpack. If solar radiation is particularly strong, the avalanche danger could rise to HIGH.
Confidence
Fair - Timing or intensity of solar radiation is uncertain on Thursday
Weather Forecast
Generally clear skies are expected for the forecast period as a ridge of high pressure becomes established over much of the province. Winds are forecast to be light to moderate from the northwest becoming southwesterly on Saturday. Daytime alpine temperatures are expected to hover between 0.0 and +5.0.
Avalanche Summary
Natural and explosive-triggered avalanches to size 3.5 were observed in the region on Tuesday. Many of the avalanches started within the recent storm snow, and then stepped down to basal facets at ground level. In 2 cases, natural cornice fall was the trigger.I would add loose wet avalanches to the mix with forecast warming. Warming may also promote ongoing persistent slab activity.
Snowpack Summary
Recent snowfall amounts were highly variable throughout the forecast area, with the western parts of the range getting as much as 90cm in the past week. The new snow sits on a variety of snow surfaces including older wind slab, a soft layer of facetted snow and/or surface hoar buried in early January.In the mid pack you may find a surface hoar layer buried in mid December. Further down you may also find the December facet/crust combo. Both interfaces give variable results in snowpack tests, but professional operators are treating them with caution.A big concern throughout the region is a layer of weak sugary depth hoar at the base of the snowpack. These crystals lie above a crust which formed in October. Several large avalanches in the past few weeks have been attributed to failures at this layer. Wide propagations on relatively gentle terrain have been noted, and an alarming tendency for seemingly disconnected slopes to propagate over a wide area and produce large avalanches.
Problems
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.
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.