Lots of new snow and wind have upped the hazard significantly. Giving the snow atleast a day or two to settle would be wise if heading into steep treeline or alpine features. Avoid any exposure to overhead slopes, avalanches may reach valley bottom.
Weather Forecast
The storm is expected to taper tonight. By tomorrow there will be mostly cloudy skies with a few early morning flurries. Alpine winds will continue to be in the moderate to high range. Temperatures will be slightly cooler tomorrow with a daytime high of -8 to -10.
Avalanche Summary
Only 1 sz2 slab was noted today on a north facing alpine area. Poor visibility prevented a good look around. It is safe to say that there is a widespread cycle ongoing in the alpine, with a specific cycle at treeline. Wind prone areas at treeline are suspect.
Snowpack Summary
As of this afternoon, the storm has left 25cm of settled snow at 2250m. This puts the total treeline snow depth to 120cm. So far the winds haven't touched the lower treeline area, but the upper treeline and alpine areas have seen a fair bit of wind and widespread slabs. The deeper instabilities (Dec 10 and Oct 26) are very pronounced and basically make up the entire bottom third. The exact burial depth of this interface will vary depending on aspect (wind loading) and elevation. The trick with this snowpack will be identifying where there is a wind slab or not. Once the storm snow has "slabbed" up expect things to become very touchy. Avalanches stepping down and/or entraining loose snow are probable.
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.
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.