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Avalanche Forecast

Archived

Nov 29th, 2021–Nov 30th, 2021

Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural and human triggered avalanches likely.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.

Regions

South Rockies.

Uncertainty around conditions is best managed through a conservative approach. Avoid recently wind loaded areas in the alpine and upper treeline.

Confidence

Low - Uncertainty is due to limitations in the field data.

Weather Forecast

Monday night: Increasing cloud. Southwest wind becoming strong. Freezing level 1900 m.

Tuesday: Flurries, up to 5 cm. Strong southwest wind. Freezing level 2000 m.

Wednesday: 10-20 cm new snow, rain below 2000 m. Strong southwest wind. Freezing level 2400 m.

Thursday: 5-10 cm overnight then clearing. Moderate westerly wind. Freezing level dropping 2000 to 1700 m.

Avalanche Summary

Neighboring Kananaskis Country reported a widespread natural avalanche cycle up to size 3 running full path on Sunday as well as a few naturals up to size 2 on Monday. Several of these large avalanches stepped down to a buried crust.

Reports in the region remain limited. If you go out in the mountains, please share your observations and/or photos on the Mountain Information Network

Snowpack Summary

With large gaps in field data, uncertainty exists around current conditions. We suspect wind pressed surfaces in the alpine and moist to wet snow treeline and below.

Two crusts are found in the snowpack: the mid-November rain crust buried 20-30 cm and reported up to 2100 m, and a crust from early November found at the bottom of the snowpack up to 2300 m, this crust is being to break down and facet. The heavy storm this week test the potential for failure on this layer.

Snowpack depths range from 40-150 cm at treeline elevations. Higher elevations may hold a deeper snowpack, but also be more heavily impacted from recent winds. Snowpack depths decrease rapidly below 1900 m.

Early season hazards are very real right now, be wary of thin/shallow snowpacks, rocks, stumps, creeks, and other sharks hidden under fresh snow.

Terrain and Travel

  • In times of uncertainty conservative terrain choices are our best defense.
  • Stay off recently wind loaded slopes until they have had a chance to stabilize.
  • Be alert to conditions that change with elevation and wind exposure.
  • Avoid shallow, rocky areas where the snowpack transitions from thick to thin.

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.