Continue to make conservative terrain choices and consider the consequences of an avalanche on a chosen slope. The snowpack remains weak and untrustworthy.
Numerous problematic weak layers exist in the middle of the snowpack, with recent observations suggesting the most likely to trigger are surface hoar layers found 40 to 80 cm deep. Be especially cautious around steep convex openings at treeline and below.
A layer of large and weak facets sits near the base of the snowpack. This layer has most recently been problematic in lower alpine elevations.
Avoid thin and rocky start zones where weak layers sit closer to the surface, riders are most likely to trigger an avalanche on this layer in terrain with shallow or variable snow depths or by first triggering a layer further up in the snowpack.
Avalanche activity has gradually slowed down after a widespread natural cycle occurred on Friday and Saturday. There were numerous large (size 2) human triggered avalanches on Sunday, and then on Monday there were fewer human triggered avalanches and they generally were smaller (size 1 to 1.5).
The previous natural cycle produced large to very large avalanches (size 2 to 3.5) at all elevations and aspects on multiple persistent weak layers. Most of the activity was on the two surface hoar layers from January, but there was also activity on the November facets near the bottom of the snowpack. Human triggered avalanches since the storm have primarily been on surface hoar layers buried 40 to 80 cm deep, many occurring in sparely forested terrain. A few large (size 1.5 to 2.5) deep persistent avalanches were triggered with heavy loads on Monday.
New snow is gradually accumulating above settled snow from last week's warm storm. At lower elevations, a rain crust exists near the surface, with reported elevations extending up to 2000 m around Nelson, 1700 m around Revelstoke, and 1600 m around Valemount.
Two persistent weak layers in the middle of the snowpack remain reactive to human triggering. They are both surface hoar layers that formed in early January and are typically found 40 to 80 cm deep throughout the Columbias. There are also some deeper facet and surface hoar layers that formed in December, but recent snowpack observations suggest they are strengthening.
The bottom of the snowpack is made up of large weak facets buried in late November, which has caused an atypical deep persistent slab problem for this region.
Tuesday night
Cloudy, isolated flurries bringing trace amounts of snow, 30 km/h southwest wind, treeline temperatures cooling to -8 °C.
Wednesday
Cloudy, light flurries with 1 to 3 cm of snow, 30 to 40 km/h southwest wind, treeline temperatures around -5 °C.
ThursdayCold front passes in the morning with 5 to 10 cm of new snow then sunny periods in the afternoon, 30 km/h northwest wind, treeline temperatures drop to -10 °C.
FridayMix of sun and cloud, 30 km/h west wind, treeline temperatures around -8 °C.
More details can be found in the Mountain Weather Forecast.
