Register for an account and never miss a forecast again!
RegisterRegister for an account and never miss a forecast again!
RegisterFeb 8th, 2020–Feb 9th, 2020
South Coast Inland.
Friday's storm delivered 20-30 cm in the south of the region and 10-15 cm in the north with changing wind direction from southwest to north. Wind slabs were created on all aspects and might still be sensitive to human triggers especially when hit by the sun.
Saturday Night: Clear, light to moderate northwest wind, alpine high -12 C, freezing level at valley bottom.
Sunday: Mix of sun and cloud, light to moderate northwest wind, alpine high -8 C, freezing level 1000 m.
Monday: Mostly sunny, light to moderate northwest wind, alpine high -5 C, freezing level 1500 m.
Tuesday: Mostly cloudy, light to moderate southwest wind, alpine high -5 C, freezing level 1000 m.
No new avalanches were reported on Thursday and Friday.
On Wednesday numerous small (size 1) natural slab avalanches were observed below treeline which released within the recent storm snow and were very soft. Several small (size 1) and one large (size 2) loose dry avalanche were reported.
The deep persistent slab avalanche activity observed during last weekend's storm in the northern portion of the region seems to have tapered off. Although the likelihood of triggering has reduced there is still concern for deep releases in that part of the region.
Friday's storm delivered 20-30 cm in the south of the region and 10-15 cm in the north. Strong southerly wind during the storm shifted to northerly wind and created wind slabs on all aspects. The snow surface is wind affected at treeline and in the alpine. The recent storm snow sits on a rain crust below 1900 m.
In the north part of the region (ie. Goldbridge/Duffey/Hurley), a few deep instabilities exist in the snowpack, including a weak basal facet crust complex. This has been the failure plane in ongoing reports of very large, deep persistent avalanches.
The south of the region, including the Coquihalla and Manning areas, currently have no concerns about deeply buried weak layers.