Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Apr 11th, 2019–Apr 12th, 2019

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.

Regions

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.

Confidence

High -

Weather Forecast

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.

Avalanche Summary

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.

Snowpack Summary

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.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.