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 15th, 2019–Mar 16th, 2019

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

Regions

South Coast Inland.

The first big warm up of spring is underway. Loose wet avalanches will be an increasing concern on Saturday. Rising temperatures and weak overnight cooling will bring our most recent weak layer back into the spotlight early next week.

Confidence

Moderate -

Weather Forecast

Friday night: Mainly cloudy. Light southwest winds. Saturday: Cloudy with sunny periods increasing over the day. Light southwest winds. Alpine high temperatures around 0 with freezing levels rising to 1900 metres and remaining elevated overnight.Sunday: Mainly sunny. Light variable winds. Alpine high temperatures around +3 as freezing levels rise to 2500 metres by end of day, increasing overnight.Monday: Sunny. Light southeast winds. Alpine high temperatures around +7 with freezing levels reaching 3300 metres and remaining elevated overnight.

Avalanche Summary

On Wednesday a skier remote triggered a size 2 wind slab on a northeast facing alpine slope at 2000 m with a crown 40 cm in depth. There are some great photos in this MIN of a size 2.5 wind slab that was skier triggered on a north facing slope on the Slalok/Matier Glacier. As we enter a period of increasing warming it's worth reminding ourselves that glide cracks are to be avoided at all times. They're incredibly unpredictable and when they fail, they often fail big. Glide avalanche concerns are especially important to consider in the Coquihalla area. A recent social media post from a professional in this part of the region does a great job of highlighting the issue. (Link here)This avalanche was reported from the Duffey Lake area on Tuesday. It indicates the nature of the bond between the recent storm snow and old surfaces below may be poor. Most other recent reports from this region have been of small loose snow avalanches.

Snowpack Summary

Light amounts of new snow have been redistributed by southwesterly and northerly winds, potentially creating some unusual wind slabs, including on south-facing slopes. Beneath this recent snow you may find hard wind-affected snow at higher elevations, soft and faceted snow in shaded and sheltered areas, and melt-freeze crusts on southerly slopes. The middle and lower snowpack is generally well-settled.

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.