South Columbia

A complex and unpredictable snowpack exists, especially in the northern half of this region. Natural and human triggered, large avalanches continue to occur.

On Tuesday afternoon we received a report of a human triggered persistent slab avalanche size 2.5 on a northerly aspect at 2000 m. On Monday, numerous natural and human triggered slab avalanches were reported up to size 2.5 with the majority failing in the recent storm snow and the deeper mid-March interface. There were several remotely triggered avalanches with the farthest being triggered from 150 m away. On Wednesday, I suspect natural avalanche activity to taper off; however, remote human triggering remains a major concern up to size 2.5. Avalanches that fail on the deeper weak interfaces will be large and destructive.

Fair - Timing of incoming weather systems is uncertain

The next Pacific frontal system will reach the coast tomorrow. The front will affect most of the Interior through the forecast period. Wednesday will see light convective flurries, moderate ridgetop winds from the SW and freezing levels near 1700 m. For Thursday, precipitation amounts expected are 10- 20 mm. Ridgetop winds will be strong from the SW and freezing levels rising to 2500 m. Warm air will remain over the region on Friday with freezing levels rising to 3000 m. Skies will show a mix of sun and cloud and ridgetop winds will be moderate strong from the SW.

At higher elevations, 40-60 cm of dense storm snow sits over the mid-March interface which had included crusts, moist snow, wind affected surfaces, and/or old wind slabs. This interface has recently come alive and is reactive, especially in the North (Revelstoke and surrounding area). Recent snowfall amounts taper off towards the south of the region. Strong SW winds had redistributed the new snow into wind slabs on leeward features. Digging deeper, 50-80 cm is the mid-February facet/crust interface. There is some concern for this layer to wake-up in the South Columbia region and storm slab avalanches have the potential to step down to it. Snow surfaces are wet to around 1700 m and moist to around 2200 m. The snow surface is undergoing melt-freeze cycles as freezing levels drop overnight.