There's a lot of uncertainty around what affect warming alpine temperatures will have. Widespread cornice failure and loose snow avalanches are likely, wind slabs may become more sensitive to triggering too. A cautious approach will serve you well.
Confidence
Low - Freezing levels are uncertain
Weather Forecast
The recent stormy pattern that December begat is history, and we enter a new meteorological regime marked by remarkable stability and a strong temperature inversion with an almost complete void of storminess over B.C for the next week. FRIDAY: No precipitation, freezing level at valley bottom with above freezing temperatures between 1600 and 2900 m, light SW winds. SATURDAY: No precipitation, freezing level at valley bottom with above freezing temperatures between 1500 and 2800 m, light SE winds. SUNDAY: No precipitation, freezing level at valley bottom, light S/SW winds. For a more detailed look at mountain weather visit avalanche.ca/weather
Avalanche Summary
On Wednesday control work produced a size 2 storm slab on a high elevation east facing feature. Previous to this, the last reported avalanche activity was on Sunday when a group of sledders triggered or remotely triggered a slab avalanche size 2.0 about 2 km south of Castle Mountain that resulted in one rider deploying his airbag and being partially buried. More details here: https://bit.ly/1TqhuQf
Snowpack Summary
As our field team travels around the region they are seeing very little wind effect. There is around 110 - 150 cm of snow on the ground at 2250 metres. The upper snowpack consists of about 40 cm of loose dry snow above 10 cm of cold facets that have been producing variable moderate to hard shears in snowpack tests. The storm snow is unconsolidated and earlier in the week the field team remarked that even the small larch trees still had new snow on them; continued evidence of very little in the way of wind. There may be more wind effect at higher elevations. These observations are consistent with reports from near Castle Mountain with storm snow above facets.
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.
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.