Avalanche Forecast

Saturday night: Cloudy with isolated flurries and a trace of new snow. Light south winds, increasing in the morning.

Sunday: Mainly cloudy with light flurries bringing up to 5 cm of new snow by end of day, continuing overnight. Light to moderate south or southwest winds, becoming strong at ridgetop. Alpine high temperatures around -4 with freezing levels to 1400 metres.

Monday: Cloudy with scattered flurries bringing up to 5 cm of new snow. Light south winds. Alpine high temperatures around -5.

Tuesday: Mainly cloudy with scattered flurries bringing up to 5 cm of new snow. Light south winds shifting west. Alpine high temperatures around -6.

Reports from Friday included several new, small (size 1) storm slab releases triggered with skier traffic and ski cutting. A couple of larger (size 2) recent natural storm slabs were also noted. North aspects figured most prominently in reports. Wet loose debris from one very large (size 3.5) avalanche was also observed in the northern Monashees. It scrubbed to ground and may have started as a slab release at around 1800 metres.

There were numerous reports over the past few days of natural and human triggered avalanches on all aspects and at all elevation bands. Most of these were size 1-2 storm and wind slab avalanches, with a few larger (size 2.5) cornice and explosives triggered storm slab avalanches.

Looking forward, now that our recent snow has formed a more reliable bond with the old surface, areas of unstable snow should become increasingly limited to recently wind loaded pockets at higher elevations.

Regular snowfall over the past week brought about 40-80 cm of snow to the region, with the greatest accumulations focused in the Monashees. 

Elevated, mainly south winds over the same period redistributed much of this snow in the alpine and upper treeline. Warm temperatures promoted slab formation with each snowfall as well as fairly quick transitions to settlement and bonding of the new snow. Surface snow is now moist or wet from warm temperatures, wet flurries, or rain up to at least 1500 metres.

The layer of surface hoar we have been tracking since late December, now buried 90 to 170 cm deep, has gained considerable strength and is now considered dormant by professionals in the region. It remains a limited concern, potentially triggerable by large loads, in isolated areas of the Selkriks and the northern end of the Monashees. It exists primarily at treeline and just below treeline.

• Avoid freshly wind loaded terrain features.
• Be alert to conditions that change with elevation, aspect and exposure to wind.