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RegisterJan 8th, 2022–Jan 9th, 2022
Kootenay Boundary.
Wind has produced deeper and more reactive deposits in lee features. Be especially mindful around steep and convex openings in the trees and ridge features in the alpine.
Saturday night: Mostly cloudy with isolated flurries. Moderate SW wind. Treeline low around -12 °C.
Sunday: Mix of sun and cloud. Moderate SW wind. Treeline high around -3 °C.
Monday: Sunny. Light and increasing S wind. Treeline high around -2 °C.
Tuesday: Incoming flurries, 5-10 cm. Moderate gusting to extreme SW wind. Treeline high around -3 °C.
A natural avalanche cycle to size 2 occurred overnight Thurs-Fri with accumulating snowfall and wind. On Friday morning, explosives easily triggered storm slabs to size 2.5.
On Wednesday, wind slabs were reactive to explosives up to size 2 in the west of the region. On Monday and Tuesday, storm slab avalanches were reactive naturally and to skier and explosive triggers, up to size 2.
There has been an alarming pattern of large, persistent slab avalanches being consistently reported over the past two weeks. Almost all of these avalanches ran on the early December weak layer. Deeply buried persistent problems like these don't go away overnight, and it remains a serious concern. Additional loading by the weight of new snow will further stress this weakness and may result in a resurgence of reactivity.
15-30 cm of new snow accumulated by the end of Friday was accompanied by southwesterly wind and warming temperatures, resulting in a denser slab forming over lower density snow. An accumulated total of 60-80 cm of new and recent snow now sits over variable and potentially weak snow surfaces including widespread facets, wind affected snow, and/or surface hoar up to 5 mm in sheltered areas.
The early December crust/facet layer has been responsible for sporadic but very large persistent slab avalanches over the past two weeks. The crust is now buried 120-200 cm deep except in thin, wind affected areas near ridgetops where nearly all of the recent avalanches have been triggered. We have uncertainty around whether new snow loads will cause this layer to fail naturally in the short term, or to help it heal in the longer term.