Avalanche Forecast

Moderate - Timing, track, or intensity of incoming weather system is uncertain on Thursday

Wednesday looks to be the last day of rather vanilla weather before a significant change Thursday. The pattern is incredibly dynamic as we move towards the weekend, this is a great time to check out our Mountain Weather Forecast (link below) if you are curious. Suffice to say that Wednesday does not offer much change, but then significant rain/snow and plenty of wind is in store, at least through Friday.WEDNESDAY: Broken cloud cover with some clearing in the late afternoon, freezing level beginning at 800 m rising to 1400 m, trace of precipitation during the day, 2 to 10 mm of precipitation expected Wednesday night. THURSDAY: Overcast, freezing level starting at 1500 m, lowering to 800 m by sundown, strong southerly wind, 15 to 20 mm of precipitation. FRIDAY: Scattered cloud cover, freezing level beginning at 500 m rising to 900 m, light southerly wind, 3 to 5 mm of precipitation possible.

Avalanche activity on Monday was limited to surface facets and surface hoar sluffing away in steep terrain.A few skier triggered soft slabs size 1 to 1.5 were reported from west facing alpine terrain Sunday. These were likely running on the mid-March crust.Saturday's reported avalanche activity was limited to sluffing and snowballing in steep terrain. There was a rather anomalous size 3.5 that was seen on the Cheakamus Glacier from Whistler last Thursday. We don't have details on the failure plane of this avalanche, but it may have run on the mid-February crust.

A new crust exists on the surface on solar aspects at all elevations. High elevation polar aspects (those facing north and east) continue to hold dry snow, this is also where trophy surface hoar up to 15 mm in size has spotted on the surface.5 to 20 cm of wind distributed snow fell last week which came to rest on the mid-March crust on all but high elevation north aspects.50 to 100 cm below the surface is a combination of facets, surface hoar, and/or crust known as the mid-February layer. This interface has not been active recently, but it does continue to produce resistant planar results in snowpack tests. The mid and lower snowpack is strong and well settled.Variable winds in the past month have built up cornices on many ridgelines. They will become touchier as daily temperatures rise and when they are subject to the strong early spring sun on clear days.