South Coast Inland

Wind slabs may linger at higher elevations. For the north of the region, be diligent around treeline, where a buried weak layer still exists. See the forecaster's blog, which describes this persistent problem: www.avalanche.ca/blogs/persistent-slab

Moderate - Due to the number of field observations

MONDAY NIGHT: Mostly cloudy with some clear breaks, lightwest wind, treeline temperature -3, freezing level in the valley bottom.TUESDAY: Mostly cloudy, light south wind, treeline temperature -3 C, freezing level 600 m.WEDNESDAY: Cloudy with isolated flurries accumulation 5-10cm, light to moderate southwest winds, treeline temperature -3 C, freezing level 700 m.THURSDAY: Mix of sun and cloud, light west winds, treeline temperature -4 C, freezing level 500 m.

No avalanches have been reported in the region over the weekend. The last large cycle was on Thursday in the north of the region, with large avalanches up to size 3. These avalanches ran within the storm snow as well as on the weak layer described in the snowpack summary.

Up to 10 cm of snow fell in the region on Sunday with associated strong winds, likely forming small wind slabs in the immediate lees of ridges. Below around 1800 m, expect the storm snow to sit on melt-freeze crust formed by rain from Thursday's storm.In the north portion of the region and possibly the far south, a weak layer of facets and surface hoar lies below all this storm snow, around 100 to 150 cm deep. The weak layer appears most prominent around treeline, up to 2000 m. While the layer is likely gaining strength, field observations show that slab avalanches remain possible on this layer where it exists. See this MIN post for snowpack test results around the Duffey on this layer.Near the base of the snowpack, a crust exists with weak and sugary facets beneath it. This could potentially still be of concern in high north-facing aspects where the snowpack rests on very smooth ground cover.