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

Dec 11th, 2011–Dec 12th, 2011

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

Regions

Northwest Coastal.

Confidence

Fair - Timing, track, or intensity of incoming weather is uncertain on Monday

Weather Forecast

15-20 cms of snow accompanied by moderate to strong southwest winds are expected for monday. Light to moderate snowfall with moderate southwest winds will continue for tuesday morning.On wednesday scattered cloud, minimal precipitation and light southerly winds are forecast for the region.Freezing levels are expected to remain at surface for the forecast period.

Avalanche Summary

No avalanche activity has been reported. Expect avalanche activity with current conditions and forecast weather.

Snowpack Summary

Between 10 and 20 cms of snow combined with strong to extreme westerly winds arrived on friday night.In some parts of the region, light amounts of new snow had previously buried large surface hoar that was sitting on a 5-20cm thick melt freeze crust. This crust extends into alpine elevations in the south, and around 1000m in the north. A strong temperature gradient in the top 30cm was reported to be faceting snow below the surface crust.The mid and lower snowpack are generally well settled and strong. At this point I have a few concerns: Because of the intensity of friday night/saturday morning's winds, the surface hoar may have been destroyed in some areas, but probably still exists in others. This makes it difficult to track now that the new snow is hiding it. As well, with the higher winds the distribution of the new wind slab may be less predictable and you are likely to find loading lower on the slope than usual. The new slab will also have varying propagation characteristics. For example, in areas where it is wind-affected and stiff, it will be likely to slide; however, you might not see the same reactivity at lower elevations or on the eastern fringe of the region where there may not have been as much wind. Regardless of all the speculation, there has been moderate snowfall with a ton of wind and it's sitting on a melt-freeze crust in a major portion of the region. With monday's forecast weather you can expect reactive windslab development in many parts of the region for the forecast period.

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.

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.