Register for an account and never miss a forecast again!
RegisterRegister for an account and never miss a forecast again!
RegisterDec 10th, 2019–Dec 11th, 2019
Sea To Sky.
Waiting for the next storm...
The snowpack structrure is unusually shallow and weak. It is still possible to trigger slab avalanches from thin spots.
TUESDAY NIGHT: Cloudy with flurries, 40 km/h wind from the southwest, alpine temperatures around -6 C, freezing level at 1200 m.
WEDNESDAY: Cloudy with flurries, 30 km/h wind from the south, alpine high temperatures around -5 C, freezing level at 1200 m.
THURSDAY: Cloudy, 20-40 cm of snow, 60 km/h wind from the southwest, alpine high temperatures around -5 C, freezing level at 1200 m.
FRIDAY: Cloudy with flurries, up to 5 cm of snow, light wind from the southwest, alpine high temperatures around -8 C, freezing level at 1000 m.
On Monday, no new avalanche activity was reported.
On Sunday, a few natural and skier triggered slab avalanches of size 1-2 were observed. Several explosive triggered slab avalanches and cornices to size 1-2 were reported. The cornices triggered small slabs on the slopes below which were up to 30 cm thick and ran on a facet/crust layer.
On Saturday, several natural avalanches up to size 2 were reported. A small slab avalanche (size 1.5) was triggered remotely by skiers on an unsupported north facing slope in the alpine. It was 20-30 cm thick.
Strong southerly winds transported the storm snow of the past week. This new snow layer is 10 - 70 cm thick depending on the amount of wind affect. Underneath this recent snow is a hard crust that formed in late November. The snow above this crust is weak and provides a bed surface for avalanches to run on. Recent snowpack tests have shown notable results on this facet/crust layer. Whumpfing and shooting cracks were reported in the alpine. The snowpack we are seeing at the moment is unusually shallow and weak for the Sea to Sky region.
Currently, typical snowpack depths in the alpine range between 50 and 180 cm, depending on the amount of wind affect. Snowpack depths taper quickly with elevation as most below treeline terrain is still below the threshold for avalanches.