Recent storm snow has probably settled and strengthened under cooler temperatures. Dense wind slabs may still be susceptible to triggering in steep lee terrain. The main snowpack feature is a rain crust buried early November and now down around 80cm at treeline. A weak layer of facets sitting on top of this crust shows "collapse" fracture character and the ability to propagate. Widespread whumpfing and cracking on this layer has also been reported. It's mostly a concern at upper treeline and alpine elevations on slopes with smooth ground cover (e.g. scree slopes, rock slabs, summer firn, grass, etc.). Coquihalla Pass and Cayoosh Pass have around 50cm on the ground at the road elevation. Treeline areas have around 100-120 cm Alpine areas likely have more snow, but also highly variable depths depending on wind exposure. For more information check out the
telemarktips.com forum, the
Mountain Conditions Report, and
Wayne Flann's Avalanche Blog.