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RegisterFeb 24th, 2021–Feb 25th, 2021
Northwest Inland.
Slabs will rapidly build with new snow and extreme wind, requiring terrain avoidance and otherwise a conservative mindset to travel safely. Treat the danger as HIGH and avoid avalanche terrain anywhere you find more than 25 cm of fresh snow.
WEDNESDAY NIGHT: Cloudy with afternoon snowfall, accumulation 10 to 20 cm, 60 to 80 km/h southwest wind, alpine temperature -11 C.
THURSDAY: Cloudy with snowfall, accumulation 5 to 15 cm, 40 to 60 km/h west wind, alpine temperature -9 C, freezing level 800 m.
FRIDAY: Cloudy with snowfall, accumulation 5 to 10 cm, 40 to 60 km/h west wind, alpine temperature -9 C.
SATURDAY: Cloudy with snowfall, accumulation 5 to 10 cm, 40 to 60 km/h west wind, alpine temperature -7 C.
We are still receiving reports of widespread avalanche activity that occurred earlier this week across the region, for example as described in this MIN as well as this MIN. We also heard of a deep persistent slab releasing out of treeline terrain on a north aspect near Ningunsaw.
Looking towards Thursday, another natural avalanche cycle may occur in parts of the region as a substantial amount of new snow and extreme wind are forecast. It will be a good day to stay well away from avalanche terrain if your local riding area has more than 25 cm of fresh snow. Should you recreate in an area with less snowfall, the safe bet will be to apply a conservative mindset and avoid slopes with any negative consequence, as triggering storm and wind slabs will remain likely.
The region may see anywhere from 15 to 35 cm by Thursday afternoon above 800 m, with associated strong to extreme southwest to northwest wind. Storm slabs are expected to build rapidly in sheltered terrain and wind slabs in exposed terrain at high elevations. Below 800 m, rain will soak a snowpack that was recently wet.
This snow will build on the 40 to 60 cm of snow that accumulated earlier this week. All of this snow overlies hard wind-affected snow in exposed terrain and weak, faceted snow or surface hoar crystals in sheltered terrain, suggesting it may take some time for the snow to bond to these surfaces.
Basal faceted snow remains part of the snowpack structure in much of the region. Once we see a substantial warm-up, we'll be thinking about the potential for the reactivation of basal layers.