Kootenay Boundary

Rising freezing levels through the day on Tuesday may begin to break down the recently formed rain crust. As the crust gradually breaks down it will be important to be increasingly cautious as deeper buried weak layers may become reactive again.

Moderate - Freezing levels are uncertain on Tuesday

TUESDAY: Cloudy with scattered wet flurries / Light to moderate east wind / Alpine temperature 2 / Freezing level 1000m rising to 2400m by late afternoonWEDNESDAY: Flurries, accumulation 5cm / Light to moderate southwest wind / Alpine temperature 1 / Freezing level 1900mTHURSDAY: Mix of sun and cloud / Light to moderate south wind / Alpine temperature -4 / Freezing level 1400m

Since the cooling weather trend there have been no reports of significant avalanche activity. That being said reports are still rolling in about the extent of avalanche activity during the rain event. Numerous large natural avalanches including size 3 and 3.5 persistent slabs were reported throughout the region failing on deep persistent weak layers at a variety of elevations and aspects.

Last weekend rain soaked the upper snowpack for a second time in a week. This time all the way to mountain tops. Cooling temperatures will have formed a 10-30cm rain crust on the surface. In parts of the region there may now be a thin layer of new snow sitting on top of the crust. Below the crust expect to see moist or wet snow. The late-February facet / surface hoar interface (70-120 cm deep), the mid-February crust (90-130 cm deep), and basal facets in shallow snowpack areas may still be present at upper elevations and may still be reactive and become a concern as surface crusts break down with daytime warming.