There is a great deal of variability across the region at this time. Several more pulses of snow and wind are expected over the next few days.
Confidence
Moderate - Intensity of incoming weather systems is uncertain
Weather Forecast
Light snow (3-5 cm) and moderate to strong westerly winds overnight with the freezing level dropping to valley bottoms. Light snow during the day Friday becoming moderate snow in the evening. Snow will be combined with moderate westerly winds and freezing levels rising up to 1400 metres. Some chance of sunny breaks during the day on Friday. Flurries or light snow during the day on Saturday with light winds and freezing levels climbing from valley bottoms up to 1400 metres. Mostly clear on Sunday with light winds and freezing levels climbing from valley bottoms up to 1400 metres.
Avalanche Summary
On Wednesday there were reports of natural cornice falls up to size 2.5, and explosives control released slab avalanches up to size 2.5. Most of the slab avalanches were in the alpine on east aspects. On Tuesday we had reports of explosives controlled slab avalanches up to size 3.0 in the west central part of the region, and thin new windslabs in the north that were skier controlled, as well as a size 2.5 deep persistent slab avalanche was reported that probably released on Monday on a west aspect in the alpine. On Monday we had reports of natural wind slab avalanches up to size 2.0, and one wind slab in the alpine that stepped down to a persistent week layer on an east aspect resulting in a size 3.0 avalanche.
Snowpack Summary
There has been 15-30 cm of new snow in the past few days that has added to the recent storm slab above the buried crust. About 25-50 cm below the surface, you'll likely find a melt freeze crust which exists in most places except for in high elevation shaded terrain. In general there seems to be a reasonable bond between the crust and the overlying snow. I'd still keep an eye on this interface as it has become reactive on some features. The early January surface hoar/ facet layer is typically down 70-120 cm. Avalanche activity at this interface has tapered-off over the past week, but I'd be reluctant to trust this potentially destructive layer just yet. In general, the lower snowpack is well settled and strong, apart from some thin snowpack areas where basal facets exist.
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.
Deep Persistent Slabs
Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.
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.