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 26th, 2022–Dec 27th, 2022

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

Regions

Vancouver Island, East Island, North Island, South Island, West Island.

Observations have been very limited and there is a lot of uncertainty about how the ongoing storm and rainfall are affecting the snowpack, so a cautious approach is advised. It is recommended to avoid steep rain-soaked areas at lower elevations and watch for new storm slab formation at the highest elevations, especially in wind-loaded terrain.

If you're out in the mountains, please consider submitting a MIN and let us know what you're seeing.

Confidence

Low

Avalanche Summary

On Sunday, observations remained limited but included several size 1 loose wet avalanches and a size 1.5 wet slab avalanche.

On Saturday, limited observations during the storm included numerous natural loose wet avalanches up to size 1.5 and several natural slab avalanches up to size 2. These slabs were up to 40 cm thick and were typically releasing at around treeline elevation. Some of these slabs were triggered by loose wet avalanches in motion.

Snowpack Summary

Rain has recently soaked the surface at all elevations. As freezing levels dropped on Monday, a new surface crust is expected to have formed. With lower freezing levels and ongoing precipitation, snowfall is expected to be burying the wet surface and/or surface crust.

Before the rainfall, new storm snow buried a highly variable old surface which included an unsupportive sun crust on southern aspects, spotty surface hoar in sheltered terrain, and heavily wind-affected surfaces in wind-exposed terrain.

A layer of decomposing surface hoar crystals could be found down 70 cm prior to the storm. There is also a layer of weak, sugary facet crystals near the base of the snowpack. During recent testing, both of these layers were producing hard results and there have been no recent reports of avalanches occurring on these layers. However, the current storm loading will test these layers and there still remains potential for avalanches in motion to step down to these older layers.

Overall, the snowpack continues to present as thin and averaged 130 cm deep at treeline prior to the storm.

Weather Summary

Monday night

Precipitation up to around 40 mm, strong to extreme SE-S wind, freezing level around 1200 m.

Tuesday

Precipitation 5-15 mm, strong S-SW wind, easing in the afternoon, freezing level reaching around 1700 m.

Wednesday

A mix of sun and cloud, moderate W wind, freezing level 800-1000 m.

Thursday

Precipitation 5-15 mm, moderate to strong S-SW wind, freezing level around 1000 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Give the new snow time to settle and stabilize before pushing into bigger terrain.
  • Make observations and assess conditions continually as you travel.
  • Be alert to conditions that change with aspect and elevation.
  • Keep in mind that wet avalanches can be destructive due to their high density.
  • A crust on the surface will help bind the snow together, but may make for tough travel conditions.

Problems

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.

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.