South Coast Inland

Any appearance of the strong April sun can initiate a loose wet avalanche cycle. The likelihood of loose wet avalanches increases as temperatures warm through the day and/or if the sun comes out for a prolonged period of time.

10-20 cm wind and temperature affected snow covers a melt-freeze crust on most slopes, and dry, faceted snow and isolated surface hoar on north-facing alpine terrain. Wind slabs have formed around upper treeline and alpine ridge crests and lee terrain features. Warm temperatures during the day are moistening the snowpack up to 2000 m; snow is rapidly melting at lower elevations. With spring conditions, the avalanche hazard will fluctuate greatly depending on the strength of the overnight freeze and how quickly the snowpack is warmed up each day.

High -

THURSDAY NIGHT: Cloudy / Light, northwesterly winds / Alpine low -4 C / Freezing level 1000 m.FRIDAY: Mix of sun and cloud / Light, westerly winds / Alpine high -2 C / Freezing level 1700 m.SATURDAY: Snow; 5-15 cm. / Moderate, southwesterly winds / Alpine high -2 C / Freezing level 1600 m.SUNDAY: Cloudy with isolated flurries; 0-3 cm. / Light, westerly winds / Alpine high -4 C / Freezing level 1400 m.

No new avalanches were reported in this region on Wednesday.A MIN report from Blowdown here documents a size 2 skier triggered wind slab avalanche on a northeast alpine aspect on Monday.A MIN report from the Whistler Backcountry here documents a similar skier triggered slab avalanche on Monday. The avalanche was triggered  on a northwesterly aspect in lee terrain below a ridge feature. While outside the forecast region, the avalanche highlights the wind slab problem that exists in the South Coast Inland.