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Avalanche Forecast

Archived

Apr 7th, 2021–Apr 8th, 2021

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

Regions

Purcells.

 Watch for isolated pockets of wind slab at upper elevations, and minimize your exposure to cornices. 

Confidence

Moderate - Uncertainty is due to the extreme variability of wind effect on the snowpack.

Weather Forecast

Wednesday Night: Cloudy with snow up 5-10 cm. Ridgetop wind moderate from the West. Alpine temperatures near -9 and freezing levels valley bottom.

Thursday: Mix of sun and cloud with isolated flurries. Ridgetop wind moderate to strong from the northwest. Alpine temperatures near -8 and freezing levels 1400 m.

Friday: Mix of sun and cloud with flurries near 5 cm. Ridgetop wind strong from the southwest. Alpine temperatures near -8 and freezing levels 1400 m.

Saturday: Mostly cloudy with some sun and 5 cm of snow. Light to moderate West wind and freezing levels 1700 m.

Avalanche Summary

On Tuesday, wet loose pinwheels were reported from steep solar aspects.

The weather pattern is spring-like which can bring intense periods of solar radiation and convective power flurries. Get after it early before daytime warming kicks in and solar radiation weakens the snowpack and cornices. Loose surface avalanches within the new snow may occur from steeper slopes and terrain features, especially if the sun comes out.

Stay well back from ridgetops that are corniced and avoid slopes with overhead cornice exposure especially under the current conditions where recent rapid growth and daytime warming has made them large and fragile. 

Snowpack Summary

5 cm to 10 cm of new snow fell across the region. Shifting wind directions from the southwest to northwest could form isolated pockets of wind slab on leeward slopes and behind terrain features. A series of melt-freeze crusts exist on all aspects below 1900 m and solar aspects to mountain top. North aspects in the alpine hold dry wintery and wind-affected snow. The mid-pack is generally strong and consolidated. 

A widespread crust layer from the mid-March warm spell can be found 30-60 cm deep, and a small surface hoar and facets have been observed at this depth on some isolated north-facing slopes. Reports suggest the snow is generally well bonded to these layers but isolated instances of large solar-triggered slab avalanches running on the crust have been observed. The early November crust is buried down 180-200 cm and has faceted crystals above and below it. This is currently dormant but something to keep in mind during the next big warm-up. 

Terrain and Travel

  • Avoid slopes when the solar radiation is strong, especially if they have large cornices overhead.
  • Watch for wind-loaded pockets especially around ridgecrest and in extreme terrain.
  • Use ridges or ribs to avoid areas of wind loaded snow.
  • Carefully evaluate bigger terrain features on an individual basis before committing to them.

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.

Cornices

Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.