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RegisterJan 28th, 2021–Jan 29th, 2021
Northwest Inland.
Moderate southwest wind will form fresh wind slabs and make it trickier to recognize older slabs which may still be reactive in the alpine.
THURSDAY NIGHT: Clear with periods of clouds, light southwest wind, treeline temperature -24 C.
FRIDAY: Mainly cloudy, up to 5 cm new snow, moderate southwest wind, treeline temperature -15 C.
SATURDAY: Mix of sun and clouds with isolated flurries, light southerly wind, treeline temperature -16 C.
SUNDAY: Mainly cloudy with isolated flurries, light southerly wind, treeline temperature -12 C.
Fresh small wind slabs and sluffing on steep alpine slopes was reported on Tuesday. Isolated large avalanches failed during the weekend storm on recently buried surface hoar in the southwest of the region where recent snowfall amounts were on the higher end (up to 15 cm). A few cornice failures were observed late last week.
Sporadic deep persistent slab avalanches were reported 1-2 weeks ago (triggered with heavy loads such as explosives and cornices), but deeper weak layers appear unreactive under the current conditions.
5-20 cm recent low density snow has buried surface hoar, which was reported as widespread below treeline and isolated at sheltered treeline and alpine locations. In some areas this new snow was redistributed by easterly winds on Wednesday and formed isolated wind slabs or soft slaps. A buried sun crust can be found on steep solar aspects. The new snow sits on widespread wind scoured surfaces, older wind slabs in alpine and exposed treeline locations and open wind effected areas below treeline. A thick crust exists near the surface below 1000 m.
The lower snowpack has two decomposing crust layers that have been causing a deep persistent slab problem for most of the past month. The upper crust is 70-140 cm deep in the Smithers area and continues to show occasional hard sudden results in snow pits. The deeper crust at the bottom of the snowpack continues to be a problem in shallow ranges like the Babines. These layers should be unreactive under the current conditions, but shallow rocky slopes should still be carefully assessed and approached with caution.
Large cornices are weakening with cold temperatures.