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Avalanche Forecast

Archived

Feb 26th, 2020–Feb 27th, 2020

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

Regions

South Rockies.

Cornice failure, loose wet avalanches and even slab avalanches are possible as the upper snowpack feels the strong sun and warming temps for the first time today. Really watch your exposure to overhead hazard, it would be easy to be surprised by weird avalanches today.

Confidence

Low - Uncertainty is due to the timing or intensity of solar radiation and its effect on the snowpack. Uncertainty is due to the fact that deep persistent slabs are particularly difficult to forecast.

Weather Forecast

Clear skies and warm sun for the next couple of days...

WEDNESDAY NIGHT: Freezing level at valley bottom, light southwest wind at lower elevations, moderate to strong northwest wind at ridge top, no precipitation expected.

THURSDAY: A few clouds, freezing level starting at valley bottom rising to about 1900 m, light southwest wind at lower elevations, strong northwest wind at ridge top, no precipitation expected.

FRIDAY: Clear skies, freezing level starting near valley bottom rising to about 2300 m, light to moderate southwest wind at lower elevations, strong southwest wind at ridge top, no precipitation expected. Freezing level holding around 1900 m Friday night.

SATURDAY: Broken cloud cover, freezing level lowering from 1900 m to 1500 m, light to moderate southwest wind, 4 to 8 cm of snow expected.

Avalanche Summary

We're short on post storm observations, but control work produced storm slabs to size 1.5 Monday and Tuesday that were most problematic near ridge crest. On Wednesday a small storm slab was reported that may have failed on surface hoar.

The most recent deep persistent slab activity we know about is described in this MIN report from February 11 and this MIN report on February 9th. This layer may become reactive again with warming temperatures and the appearance of the strong late winter sun.

Snowpack Summary

The 10 to 35 cm of snow from Sunday/Monday has been absolutely hammered by wind Wednesday as evidenced in this MIN submission. Wind was strong enough to get into below treeline features even. Wind stiffened slabs now rest on a variety of old surfaces including a firm crust on solar aspects, soft faceted snow, possibly surface hoar in sheltered areas, and old wind slabs near ridge crest. 

A thick rain crust sits 30-60 cm below the surface and can be found up to 2100 m. Avalanche activity was last observed at the faceting interface between this crust and overlying snow on February 17. 

The mid-pack is well settled and strong, but the base of the snowpack contains basal facets that are most prominent in shallow rocky start zones.

Terrain and Travel

  • Avalanche hazard is expected to to increase througout the day, think carefully about your egress.
  • Avoid freshly wind loaded features, especially near ridge crests, roll-overs and in steep terrain.
  • Use extra caution around cornices: they are large, fragile, and can trigger slabs on slopes below.
  • Recent wind has varied in direction so watch for wind slabs on all aspects.
  • The likelihood of deep persistent slab avalanches will increase with each day of warm weather.

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.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.