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Avalanche Forecast

Archived

Jan 25th, 2021–Jan 26th, 2021

Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

South Rockies.

There is little change right now with trace amounts of new snow and light winds. Nonetheless, keep in mind those classic Rockies hazards: shallow rocky snowpacks, stubborn hard wind slabs, cornices and variable wind-loading patterns.

Confidence

High - Confidence is due to a stable weather pattern with little change expected.

Weather Forecast

Another day of cloudy cool conditions before some forecasted light snow mid-week.

MONDAY NIGHT: Mainly cloudy with clear periods, light southwest wind, treeline temperatures around -12 C.

TUESDAY: A mix of sun and clouds with isolated flurries, trace new snow, light south wind increasing to moderate late afternoon, treeline temperatures around -13 C.

WEDNESDAY: Mainly cloudy with scattered flurries, trace to 5 cm new snow, light to moderate southeast wind, treeline temperatures around -13 C.

THURSDAY: Mainly cloudy with scattered flurries, trace to 5 cm new snow, light southerly wind, treeline temperatures around -13 C.

Avalanche Summary

No recent avalanches have been reported aside from loose dry avalanches (sluffs) from steep alpine and treeline terrain from the neighbouring Lizard Range forecasting area. Cornices are growing fragile with continued cold conditions faceting their bonds. 

Snowpack Summary

Alpine and upper treeline terrain remains heavily wind affected from last week's strong to extreme southwest winds with scouring, sastrugi, isolated pockets of soft snow and layers of hard wind slab. A hard thick crust is found below 1800 m. Near-surface faceting continues to slowly soften hard surfaces and weaken cornices. 

A solid mid-pack sits above deeply buried decomposing crust and facet layers near the bottom of the snowpack (100-150 cm deep). Avalanche activity on these layers has been sporadic and mostly triggered by large loads such as wind slab avalanches and cornice falls. Though unreactive under the current conditions, steep rocky slopes and shallow snowpacks should still be carefully assessed and approached with caution.

Terrain and Travel

  • Watch for wind-loaded pockets especially around ridgecrest and in extreme terrain.
  • Small avalanches can have serious consequences in extreme terrain. Carefully evaluate your line for wind slab hazard before you commit to it.
  • Pay attention to cornices and give them a wide berth when traveling on or below ridges.

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.