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Avalanche Forecast

Archived

Mar 15th, 2022–Mar 16th, 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 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, human triggered possible.

Regions

North Rockies.

Wind slabs are expected to remain reactive to human-triggering. Avoid wind-loaded areas and watch signs of instability.

Choose conservative, low consequence lines. Riders have been surprised in recent days by large avalanches failing on a weak layer of surface hoar.

Confidence

Moderate - Uncertainty is due to the fact that persistent slabs are particularly difficult to forecast.

Weather Forecast

A series of frontal systems coming in off the coast will bring light precipitation throughout the week.

Tuesday Overnight: Mainly cloudy, light precipitation. Localized areas up to 10 cm accumulation. Moderate to strong westerly winds. Freezing level dropping to 900 m. 

Wednesday: Partially cloudy, light precipitation. Localized areas up to 10 cm accumulation. Moderate to strong westerly winds. Freezing level rising to 1500 m.

Thursday: Mainly cloudy, light precipitation. Moderate to strong westerly winds. Freezing level 1500 m.

Friday: Partially cloudy, light precipitation. Moderate to strong southwesterly winds. Freezing level rising to 1500 m.

Avalanche Summary

On Monday, several natural wind slabs were reported on easterly aspects at treeline as strong winds redistributed the new snow. A few natural wet loose avalanches occurred at treeline and below as a result of solar radiation and warm temperatures. 

Numerous natural and sledder-triggered avalanches were reported throughout the weekend in the Pine Pass area down 25-70 cm, all failing on surface hoar. The most reactivity has occurred on wind-loaded, northeast aspects. Most notably, a size 2.5 sledder-triggered avalanche occurred near Bijoux Falls. The full report can be seen here.

A few sledder-triggered avalanches up to size 2 were reported in the Renshaw area on Sunday. These storm slabs were failing on a weak layer of surface hoar down 25-40 cm.

Snowpack Summary

Continued light precipitation will add to 30-60 cm of recent settling storm snow. In the alpine and treeline, southwest winds have redistributed the new snow into wind slabs in lee areas. Below treeline, moist snow or a melt-freeze crust can be expected from rain and warm temperatures.

This new snow is sitting on various surfaces, including hard wind-affected snow, sun crusts on southerly slopes, and most notably large surface hoar on shady or sheltered slopes. This layer of surface hoar is expected to remain problematic in the coming days, with the most reactivity observed in the Pine Pass and Renshaw area.

The mid and lower snowpack is generally well-settled and strong in most areas, with multiple crusts throughout. No recent persistent slab avalanches have been reported on these layers.

Terrain and Travel

  • Avoid freshly wind loaded features, especially near ridge crests, roll-overs and in steep terrain.
  • Continue to make conservative terrain choices while the storm snow settles and stabilizes.
  • Potential for wide propagation exists, fresh slabs may rest on surface hoar, facets and/or crust.
  • Carefully assess open slopes and convex rolls where buried surface hoar may be preserved.

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.

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.