Sea To Sky

New snow amounts within this region will be highly variable on Saturday with more snow in the south. Hazard may be one step lower in areas that receive less than 25 cm of new snow.

Moderate - Forecast snowfall amounts are uncertain on Saturday

SATURDAY: 20-30 cm of new snow / Strong southwesterly ridgetop winds / Freezing level rising to around 1000m.SUNDAY: 20-30 cm of new snow / Strong southwesterly ridgetop winds / Freezing level rapidly rising to around 1800m.SUNDAY NIGHT: 15-25 cm of new snow / Strong southwesterly ridgetop winds / Freezing level around 1800m.MONDAY: 25-30 cm of new snow / Strong to extreme southwesterly ridgetop winds / Freezing level around 1800m.

Throughout this region there has been evidence of a natural avalanche cycle up to size 3 that occurred within the storm snow on Wednesday. More notable are the numerous explosive triggered, very large avalanches up to size 3.5 that where reported near Whistler on Thursday. These avalanches started in the storm snow and then stepped down to the early January and even the mid-December crusts which resulted in very large avalanches running full path. They occurred on northwesterly aspects below rocky ridgetops at around 1950 m. Although these layers are over 200 cm beneath the snow surface, a large trigger such as a falling cornice or a smaller human triggered avalanche could very likely "step-down" to these layers resulting in large and destructive avalanches.

15-20 cm of new snow on Thursday morning brings recent storm totals to around 60-80 cm which continues to be redistributed by strong southeasterly winds. Last weekend's storm created dense storm slabs lurking in lee and cross-loaded features. Impressive cornice growth has also been observed on the lee side of ridgetops. 200-250 cm below the surface you'll find a crust that was buried early January and is present at all elevations. Below this there is another crust which was buried in mid-December. Recent explosive control work has triggered storm slab avalanches that have then "stepped-down" to both of these crusts, resulting in very large avalanches running full path. Although these layers are over 200 cm beneath the snow surface, a large trigger such as a falling cornice or a smaller human triggered avalanche could very likely "step-down" to these layers resulting in very large and destructive avalanches.