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

Jan 3rd, 2022–Jan 4th, 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 possible, human triggered probable.
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 unlikely, human triggered possible.

Regions

Purcells.

Newly formed storm slabs are expected to be touchy on Tuesday. The region continues to deal with a tricky persistent slab problem and very large avalanches remain possible. Conservative terrain selection remains critical.

Confidence

High -

Weather Forecast

Unsettled conditions are expected on Tuesday in the wake of the storm. Periods of light snow and periods of sun are both possible. 

Monday night: Snowfall 5-10 cm, moderate to strong SW wind, treeline temperature around -10 °C. 

Tuesday: A mix of sun and cloud with periods of flurries, light to moderate SW wind, treeline high around -10 °C. 

Wednesday: A mix of sun and cloud with a chance of flurries in the morning, light to moderate N wind, treeline high around -12 °C. 

Thursday: Snowfall 2-6 cm, moderate to strong SW wind, treeline high around -12 °C. 

Avalanche Summary

Early reports from Monday include natural size 1 winds slabs and explosive triggered storm slabs up to size 2. This MIN report from the south of the region shows an example of the instability in the storm snow and good decision making. 

There has been consistent reports of persistent slab avalanches on reloaded bed surface crusts from the Invermere area over the past month. On Sunday, one of these events was reported on a N aspect in the alpine. On Thursday, a size 1 was triggered remotely by bootpacking on a thin northeast aspect in the alpine. Explosive control work on December 26th produced large avalanches (size 2) on the crust found 40-70 cm deep.

On Tuesday, recently formed slabs are expected to remain reactive to human triggering. These new slabs sit on a weak interface and may be very reactive, especially in wind loaded terrain. In the areas that received more than around 25 cm, the new slabs are expected to be widespread while in the areas with less new snow, the problem will likely be isolated to wind loaded areas. The persistent slab problem remains a serious concern and the weight of the new snow may increase the reactivity of these deeper layers. Smaller storm slab and wind slab avalanches also have the potential to step down to deeper layers resulting in very large avalanches. 

Snowpack Summary

The new storm snow buried a variable snow surface which is likely weak and includes widespread facets, wind affected surfaces, and/or surface hoar up to 3 mm in sheltered areas. The new snowfall was accompanied by moderate to strong winds and new storm slabs are expected to be most reactive in wind loaded areas. 

The most notable layer of concern in the snowpack is a crust that was formed in early December and is now down 70-150 cm. Activity on this layer has been sporadic. It has generally been triggered on steep, rocky slopes, with a shallow or thin-to-thick snowpack. This layer has created a low likelihood, high consequence scenario which is best managed through conservative terrain choices and disciplined backcountry travel techniques.

A late October facet/crust layer sits at the bottom of the snowpack above 1900 m. 

Terrain and Travel

  • Continue to make conservative terrain choices while the storm snow settles and stabilizes.
  • Be aware of the potential for large avalanches due to the presence of a persistent slab.
  • Avoid steep, rocky, and wind effected areas where triggering slabs is more likely.

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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.