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RegisterMar 3rd, 2021–Mar 4th, 2021
Cariboos.
Conservative decisions and sticking to simple low angle terrain is strongly recommended. The combination of warm temperatures and a weak snowpack structure is dangerous.
A short lived ridge will bring dry warm weather on Thursday.
WEDNESDAY NIGHT: Partly cloudy, moderate south wind, treeline temperatures drop to -5 C.
THURSDAY: Mix of sun and cloud, strong south wind, freezing level climbs to around 1800 m with treeline temperatures around -1 C.
FRIDAY: Cloudy with scattered flurries and 5-10 cm of new snow, strong south wind, freezing level climbs to 1700 m with treeline temperatures around -2 C.
SATURDAY: Another 5 cm of new snow by the morning then a mix of sun and cloud during the day, light southwest wind, freezing level climbs to 1400 m with treeline temperatures around -5 C.
While we are uncertain about the current reactivity of persistent slab problems in the Cariboos, the combination of an overall weak snowpack structure with warming temperatures and sunshine suggest this is a time to be extra cautious in avalanche terrain. Read the latest Forecaster Blog for concerns about the warming.
Although there have been limited recent field observations, we have good reason to remain suspect of persistent weak layers producing large destructive avalanches. On Sunday, there was a report of a size 2 human-triggered wind slab avalanche in the east of the region (MIN report) and this MIN report from just north of the region in the McGregors shows a very large (size 3.5) persistent slab avalanche that likely occurred on Sunday as well. There were several significant reports of avalanche activity last week between Feb 23 and Feb 25 including:
Surface conditions are a mix of wet and crusty snow at low elevations and south-facing slopes, hard wind affected snow at upper elevations, and settling powder in some shaded and sheltered terrain.
Over the past few weeks there have been multiple deeper weak layers producing large avalanches, but we have little to no information about how these layers have trended over the past few days. Layers of concern include a 50-100 cm deep layer of facets that was buried in mid-February, a 50-150 cm deep layer of surface hoar from early February that was most prevalent at treeline (and existed as a facet/crust combination on steep south-facing terrain), and finally another persistent weak layer from late January that is now roughly 100-200 cm deep.