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RegisterDec 21st, 2021–Dec 22nd, 2021
Vancouver Island.
10 to 25 cm is inbound Tuesday night with another 10 to 20 cm expected Wednesday, all of it is set to arrive with strong to extreme wind out of the southwest. New slabs may be forming on surface hoar, especially in open areas at mid and lower elevations. Avoid avalanche terrain.
Batten down the hatches friends, big wind and plenty of precipitation is headed our way…
TUESDAY NIGHT: Freezing level around 1800 m at sundown, lowering to about 1000 m by day break, 10 to 25 cm of snow at upper elevations and rain down low, strong to extreme southwest wind.
WEDNESDAY: Overcast, freezing level lowering from 1000 m to 500 m throughout the day, strong to extreme southwest wind, 10 to 20 cm of snow up high with rain at lower elevations.
THURSDAY: Broken cloud cover, freezing level around 400 m, moderate to strong northwest wind, no precipitation expected during the day, 2 to 10 cm possible Thursday night.
FRIDAY: Broken cloud cover, freezing level just above sea level, light to moderate southwest wind, no precipitation expected.
No new avalanche observations to report. As new snow and wind come together Tuesday night into Wednesday, we will likely see some avalanche activity in the new storm snow, especially in areas where it stays cold enough for new snow to fall on surface hoar.
Widespread surface hoar has been observed on top of the 20 to 50 cm of premium powder snow that fell last weekend, as evidenced in this MIN, and this MIN from our field team. During that storm, higher snow totals accumulated in the southwest of the region. Temperatures warmed slightly at upper elevations on December 21st, Upper Cruikshank reported +2 C at 1348 m Tuesday afternoon.
A gradual temperature rise may have formed a crust layer within the storm snow in areas below 1000 m in the northern half of the region and closer to 1200 m in the southern half.
Below a meter of snow from mid-December storms, two crust layers can be found that formed in early December. Small facets (sugary snow) had been reported near these crusts that are likely trending unreactive. Below these crust layers, the snowpack is generally well-settled. Early season hazards such as rocks, stumps, and open creeks remain at lower elevations.