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Avalanche Forecast

Archived

Mar 15th, 2022–Mar 16th, 2022

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

Regions

Purcells.

Wind slab avalanches are possible at upper elevations in the wake of the warm storm. Expect conditions to change dramatically with elevation and aspect.

Confidence

Moderate - Uncertainty is due to the complexity of the snowpack’s structure.

Weather Forecast

TUESDAY NIGHT: Cloudy with isolated flurries bring trace amounts of snow to most parts of the region and up to 5 cm along the western slopes, moderate wind from the west, treeline temperatures cool to -8 C.

WEDNESDAY: Mostly cloudy skies with some isolated flurries and trace amounts of precipitation, moderate wind from the west, treeline temperatures around -4 C with freezing level around 1500 m.

THURSDAY: Mix of sun and cloud, moderate to strong wind from the southwest, treeline temperatures up to -2 C with freezing level climbing to 1800 m.

FRIDAY: Cloudy with flurries easing off in the morning bringing up to 5 cm of new snow, light wind from the southwest, freezing level around 1600 m.

Avalanche Summary

There have been several reports of small (size 1 to 1.5) human triggered slab and loose avalanches over the past few days. These have mostly been on steep wind-loaded north and east facing slopes. Wind slabs likely grew during the stormy weather on Tuesday, and will remain possible to trigger over the upcoming days.

Snowpack Summary

The most recent storm delivered 15 cm along the eastern Purcells and up to 30 cm along the western Purcells. This snow is likely settling relatively quickly, although could remain reactive in wind-affected terrain. The surface is likely moist and crusty below 1500 m. Several crusts can be found in the top 60 cm of the snowpack. Recent observations suggest the snow is generally well bonded to these crusts, but there could be isolated areas where these could be reactive so pay attention to signs of localized instability such as whumpfing or cracking.

Terrain and Travel

  • Be careful with wind loaded pockets, especially near ridge crests and roll-overs.
  • Wind slabs may be poorly bonded to the underlying crust.
  • Be alert to conditions that change with aspect and elevation.
  • Watch for signs of instability like whumpfing, hollow sounds, shooting cracks or recent avalanches.

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.