Register for an account and never miss a forecast again!
RegisterRegister for an account and never miss a forecast again!
RegisterJan 4th, 2022–Jan 5th, 2022
South Columbia.
The best riding and lowest hazard intersect in wind sheltered terrain below treeline. If you're stepping out into wind affected terrain, you'll likely find storm slabs that are sensitive to human triggering. Keep your terrain choices in check as the storm snow settles.
Another storm is set to impact the region Thursday.
TUESDAY NIGHT: Overcast, freezing level at valley bottom, trace of snow possible, light variable wind.
WEDNESDAY: Broken cloud cover, daytime high temperature between -10 and -15 C at treeline, light wind generally out of the northwest, trace of snow possible.
THURSDAY: Overcast, daytime high temperature between -10 and -15 C at treeline, strong southwest wind, snow beginning in the morning, 5 to 15 cm expected during the day with another 5 to 15 cm expected Thursday night.
FRIDAY: Overcast, flurries, daytime high temperature between -10 and -15 C at treeline, strong west/southwest wind, 5 to 10 cm of snow possible.
Lots of natural (and a few human triggered) storm slabs and loose dry avalanches to size two were observed Monday, primarily on northeast facing terrain.
In both the North and South Columbias avalanche activity on the early December crust/facet interface has really tapered over the last week. It has been confined to a couple of isolated avalanches in complex northeast facing alpine terrain. Two were explosive triggered, while one failed naturally. Each had wide propagation and ran several hundred metres.
Cornice falls have triggered numerous slabs recently. Navigate around cornices carefully, both on ridgelines and on the slopes below.
The weekend storm produced 20 to 50 cm of storm snow accompanied by wind that was quite variable, but mainly out of the south. Wind loading is suspected to be extensive in the alpine, but the bulk of the observations we're getting are from lower elevations.
We're actively monitoring the early December crust. In some places it's scoured and on the surface, while in wind loaded terrain features it can be found as deep as 150 cm below the surface. It consists of faceted grains above a bulletproof crust formed by the Atmospheric Rivers of early December. Avalanches failing on this interface have the potential to be very large. There has been isolated avalanche activity on this crust in the last week that seems to be confined to complex alpine terrain.
The biggest concern is how it will behave next weekend as temperatures rise quite dramatically.