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Avalanche Forecast

Archived

Jan 13th, 2022–Jan 14th, 2022

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

Regions

Purcells.

Dial back your exposure to avalanche terrain when temperatures increase. Large avalanches are possible as buried weak layers adjust to the warming.

Confidence

Moderate - Uncertainty is due to how the snowpack will react to the forecast weather.

Weather Forecast

THURSDAY NIGHT: Partly cloudy, no precipitation, moderate wind from the northwest, treeline temperatures cool to -4 C with freezing level dropping somewhere below 1500 m.

FRIDAY: Mix of sun and cloud, no precipitation, light wind from the northwest, treeline and alpine temperatures around -2 C with freezing level around 1200 m.

SATURDAY: Mostly cloudy with isolated flurries, trace amounts of new snow, moderate wind from the southwest, treeline temperatures around -2 C with freezing level around 1200 m.

SUNDAY: Mostly sunny skies, no precipitation, moderate wind from the west, treeline temperatures around -4 C.

Avalanche Summary

Wednesday's storm resulted in some small (mostly size 1) slab avalanches in the top 15 cm of new snow. Explosive control in the Invermere area produced a few size 2 avalanches that failed on the early December persistent weak layer. These occurred on relatively shallow northeast-facing slopes at 2000 m, where the layer was buried 60-80 cm deep.

We have seen sporadic avalanche activity on this persistent weak layer since Jan 4. These have included some large human triggered avalanches, such as this size 3.5 avalanche just outside the region at Pedley Pass on Jan 4 and this avalanche near Golden on Jan 9, as well as large natural avalanches like this one reported in the South Purcells on Jan 9. These avalanches suggest the persistent slab problem is an ongoing concern in the Purcells.

Snowpack Summary

15 cm of recent snow is rapidly settling, with surfaces at lower elevations likely going through a daily melt-freeze cycle. Dry snow can likely be found in alpine terrain, although it will likely be wind-affected. This most recent snow has buried some small surface hoar and melt-freeze crusts. The snow should bond to these layers relatively quickly, but could remain unstable in isolated pockets. The most notable layer of concern in the snowpack is a crust that was formed in early December and is now down 90-160 cm. Activity on this layer has been sporadic, but has generally been triggered on steep, rocky slopes, with a shallow or thin-to-thick snowpack.

Terrain and Travel

  • The more the snowpack warms-up and weakens, the more conservative you`ll want to be with your terrain selection.
  • Be aware of the potential for large avalanches due to the presence of a persistent slab.
  • Avoid shallow, rocky areas where the snowpack transitions from thick to thin.
  • Use ridges or ribs to avoid areas of wind loaded snow.

Problems

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.

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.