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RegisterMar 13th, 2020–Mar 14th, 2020
Kootenay Boundary.
New snow and strong east wind will form new wind slabs in exposed terrain. This snow is continuing to load buried weak layers that have surprised people.
FRIDAY NIGHT: Cloudy with snowfall, accumulation 5 to 10 cm, moderate to strong east wind, alpine temperature -17 C.
SATURDAY: Cloudy with snowfall then clearing, accumulation 2 to 5 cm, light to moderate east wind, alpine temperature -16 C.
SUNDAY: Clear skies, light northeast wind, alpine temperature -10 C.
MONDAY: Clear skies, light northeast wind, alpine temperature -5 C, freezing level rising to 1500 m.
A few wind slab avalanches were triggered by humans on Friday. They were in alpine terrain and on north and east aspects, about 40 cm deep. One of the wind slabs stepped down to the surface hoar layer described in the Snowpack Summary.
Many wind slab avalanches were triggered by explosives and naturally on Thursday. They occurred on all aspects, at alpine elevations, and were 20 to 40 cm thick.
Widespread avalanche activity is starting to quiet down on the surface hoar layer described in the Snowpack Summary. Over the past two weeks, small to large (size 1 to 2) avalanches have released on this surface hoar layer. They have most often released between 1800 and 2300 m on northwest to east aspects.
Snowfall and strong easterly wind will form new wind slabs in exposed terrain. This wind direction is atypical, so terrain features that don't typically have wind slabs may this weekend. Wind slabs may still linger in north to east terrain from the storm earlier in the week.
The upper snowpack is relatively complex. A few different layers of surface hoar and melt-freeze crust exist, which have recently acted as sliding layers. One such layer buried about a week ago may be found about 20 to 40 cm deep. The most widespread layer was buried late February and is now buried 60 to 80 cm. This layer is most commonly found in open trees (e.g. in this MIN) or sheltered terrain around the upper part of below treeline, treeline, and lower alpine elevations. This layer may only remain a concern in the north and east parts of the region.
The remainder of the snowpack is strong and well-settled.