North Columbia

Warming temperatures have settled the recent storm snow into a cohesive slab sitting on weak facets (sugary snow) that is ripe for human triggers; intense solar radiation will increase the likelihood of human triggered avalanches.

Moderate -

FRIDAY NIGHT: Partly cloudy with some clearing / Light, westerly winds / Alpine low -6 / Freezing level below valley bottom.SATURDAY: Partly cloudy in morning becoming mostly sunny / Light, westerly winds / Alpine high 2 / Freezing level rising to 1700 m.SUNDAY: Sunny / Light, northwesterly winds / Alpine high 4 / Freezing level rising to 2100 m.MONDAY: Sunny / Light, northwesterly winds / Alpine high 6 / Freezing level rapidly rising to 2900 m.

On Thursday, a rider triggered size 2.5 persistent slab avalanche was reported on a west aspect at 2000 m. Another rider triggered size 2 persistent slab avalanche was triggered from 50 m. away from the slope that avalanched. It was a southwest aspect at 2300 m. Human triggered persistent slab avalanche activity is expected to increase with the forecast sunshine and rising freezing levels.On Wednesday, numerous natural storm slab avalanches up to size 3 and rider triggered up to size 2 were reported on all aspects at treeline and above. Some of the avalanches were triggered remotely from lower angle terrain by skiers 30 m. away from the slope that avalanched. This suggests that recent storm snow is still very sensitive to human triggers in specific locations.

10-15 cm of new snow brings the recent storm snow to 40-60 cm. This snow is sitting on a pile of facets (sugary snow), as well as a crust on sun exposed slopes. The recent storm snow has settled into a cohesive slab and is ripe for human triggering. This persistent slab is currently our primary concern.At lower elevations, a weak layer of surface hoar (weak, feathery crystals) buried in mid-January can be found approximately 70-120 cm deep. This layer has recently been unreactive, however, the forecast warming event may awaken this layer in low elevation areas such as steep cutblocks and large open glades.The lower snowpack is generally considered to be strong, except for shallow, rocky areas in the alpine.