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

Mar 1st, 2019–Mar 2nd, 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.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Northwest Inland.

The Northwest Inland is in for a cold and sunny weekend. Keep in mind the potential to encounter wind slabs at upper elevations, which may be reactive to human triggers.

Confidence

Moderate -

Weather Forecast

FRIDAY NIGHT - Clear with cloudy periods / east winds 10-15 km/h / alpine low temperature near -19SATURDAY - Mainly sunny / east winds 15-25 km/h / alpine high temperature near -18SUNDAY - Sunny / east winds 20-40 km/h / alpine high temperature near -13MONDAY - Sunny / east winds, 20-30 km/h / alpine high temperature near -7

Avalanche Summary

On Thursday, there were reports of several loose avalanches up to size 1.5 that were triggered by the sun on steep south facing slopes. A few of these loose avalanches triggered small slab avalanches, up to size 1.5.On Wednesday, there were several reports of wind slab avalanches to size 1.5, and one size 3 occurring on a south aspect at 2000 m. There were also reports of loose avalanches being triggered by the sun on steep, south facing terrain.

Snowpack Summary

Recent strong winds have formed wind slabs in the alpine and at treeline. Due to variable wind directions, wind slabs may be found on all aspects. The snow surface is likely a crust on south facing slopes.Soft snow can still be found in sheltered terrain, and in most areas, 20-50 cm of snow sits on old wind slabs and a crust on south facing slopes. In some sheltered areas, this snow sits on facets (sugary snow) and surface hoar (feathery crystals).In the south of the region, the lower snowpack is considered generally strong. In the north of the region, there may be a layer of surface hoar and facets buried approximately 50 cm.

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.