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Avalanche Forecast

Archived

Mar 4th, 2021–Mar 5th, 2021

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

Regions

Kananaskis.

It sure felt like spring today! It warmed up significantly today, there will be a new crust on sunny aspects. Expect another warm day tomorrow. Travel early, finish early and anticipate a quick deterioration in the snowpack when the warmth arrives. 

Confidence

High -

Weather Forecast

After a warm day on Thursday, we can expect a slight re-freeze tonight, followed by another warm day tomorrow. The overnight low will be around -5, and by noon temperatures will approach zero. Blue skies will stick around for Friday and winds will be light from the SW. Later in the wee we are expecting some snow.

Avalanche Summary

A few small loose wet avalanches on EEOR today. Mt Sparrowhawk had a more notable sz2 loose wet on a southern aspect.

Snowpack Summary

Given the warm day, expect a crust on southern aspects and possibly even western aspects. Recent snow from earlier in the week is settling. This snow is overlying a windslab down 10-20cm that was seeing some isolated cracking today in the Aster lake area. Deeper in the snowpack there are two layers that we are following closely. The Feb 19th Facets down 40-60cm and the Jan 29th interface down 60-100cm. Windslabs (buried and near the surface) in the upper snowpack are likely to step down to one of these layers that are within the top meter. These layers are subtle at treeline but very pronounced in the Alpine. Dig down and assess these layers. Forecasters today avoided big slopes in the alpine due to windslabs over these interfaces. Moist snow was also found up to 2000m by midday.  

Terrain and Travel

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Avoid lee and cross-loaded terrain.
  • Pay attention to isolated alpine features as well as cross-loaded features at treeline.
  • Be alert to conditions that change with elevation and sun exposure.
  • Avoid sun exposed slopes when the solar radiation is strong, especially if snow is moist or wet

Problems

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.

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.