Register for an account and never miss a forecast again!
RegisterRegister for an account and never miss a forecast again!
RegisterJan 23rd, 2020–Jan 24th, 2020
South Coast Inland.
Be prepared to avoid avalanche terrain if there's heavy snowfall in your part of the region, snowfall amounts are highly variable.
THURSDAY NIGHT: Flurries continue overnight bringing another 10-20 cm of snow, strong wind from the southwest, freezing level drops to 1500 m with alpine temperatures around -2 C.
FRIDAY: Scattered flurries as the front leaves the region with most areas getting 5-15 cm of new snow and a few (uncertain) locations likely getting 15-25 cm, moderate to strong wind from the southwest, alpine temperatures around -3 C.
SATURDAY: Cloudy with some light flurries, light wind from the southwest, alpine high temperatures around -3 C.
SUNDAY: Mix of sun and cloud with light flurries starting in the afternoon, moderate wind from the south, alpine high temperatures around -3 C.
There are no reports since the onset of the current storm, but it has likely caused natural storm slab avalanches in parts of the region that have received more than 20 cm of new snow. The additional load of new snow is also increasing the likelihood of deep persistent slab avalanches in northern parts of the region.
A frontal system crossing the region is resulting in variable amounts of new snow and forecast amounts on Friday are also variable and uncertain. As of Thursday afternoon the northern part of the region received 15-30 cm and the southern part of the region received 10-15 cm. Another 15-40 cm of snow could accumulate by Friday afternoon, resulting in very thick and widespread storm slabs in some areas and more localized wind slabs in other areas. Wind over the past few days has been strong from the south, resulting in highly variable conditions in open terrain.
There are currently no concerns about deep weak layers in the south of the region (e.g. Coquihalla).
There have been two layers of concern in the northern half of the region (e.g. Duffey, Hurley). One is a weak layer of surface hoar buried about 100 cm deep that professionals are tracking at treeline in sheltered areas. The other is weak faceted grains and crusts near the bottom of the snowpack, that is most likely to be triggered in shallow rocky start zones.