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Avalanche Forecast

Archived

Apr 17th, 2021–Apr 18th, 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 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 Columbia.

Yet another day without a good overnight refreeze. Temperatures will drop in the morning, but sun exposure can deteriorate conditions rapidly. The rating is for the hottest time of the day.

Check out the Forecaster's Blog on warming and how to stay safe.

Confidence

Moderate - Uncertainty is due to how quickly the snowpack will recover and gain strength.

Weather Forecast

The high pressure ridge is forecast to break down Sunday morning bringing light precipitation and lowering freezing levels followed by a classic diurnal melt-freeze cycle on Monday for the next couple of days.

Saturday night: Clear with increasing cloud coverage towards the morning, light to moderate northwest wind, alpine low +1 C, freezing level at 3000 m and lowering to 2500 m in early morning hours.

Sunday: A few clouds with isolated flurries in the morning and mainly sunny from mid-morning onward, trace of new snow and rain below treeline, moderate to strong northeast wind, alpine high +2 C, freezing level dropping to 1700 m in the morning.

Monday: Mainly sunny, light to moderate northerly wind, alpine high +4 C, freezing level 2000 m.

Tuesday: Mainly sunny, light variable wind, alpine high +7 C, freezing level 2300 m.

Avalanche Summary

On Friday numerous wet loose avalanches on all aspects and wet slabs to size 3 on solar aspects were reported. Numerous wet loose avalanches to size 2 were observed on steep solar aspects on Thursday and Wednesday (see this MIN). Several wet slab avalanches of size 2.5-3 and one size 3.5 were reported on Thursday. 

A few recent natural cornice failures of size 2.5 did not trigger slabs on slopes below.

Several glide cracks opened up and glide snow avalanches released with the warm temperatures. Glide slabs are hard to predict and can release at any time, so it is important to avoid slopes with glide cracks. 

Snowpack Summary

The snow surface consists of a melt-freeze crust on solar aspects and shaded aspects up to 2200 m which transitions into moist/wet snow during the day. Dry snow might still be found on northerly aspects in the alpine above 2400 m. 20-30 cm of recent snow has formed isolated pockets of wind slab on leeward slopes and behind terrain features. The recent snow sits on a series of melt-freeze crusts on all aspects below 1900 m and southerly aspects to mountain top. On North aspects in the alpine, the recent snow sits on dry wintery snow surfaces and possibly surface hoar on wind-sheltered slopes. 

Cornices are large, fragile and failing with warm temperatures. Several natural cornice falls were observed recently. 

Recent periods of warm weather are expected to have helped old persistent weak layers heal, including a few crusts buried over the last month as well as a facet layer 150 cm deep from the mid-February cold snap. 

Terrain and Travel

  • Use extra caution around cornices: they are large, fragile, and can trigger slabs on slopes below.
  • Avoid slopes when the solar radiation is strong, especially if they have large cornices overhead.
  • Avoid sun exposed slopes, especially if snow surface is moist or wet.
  • Small avalanches can have serious consequences in extreme terrain. Carefully evaluate your line for wind slab hazard before you commit to it.

Problems

Wet Slabs

Wet Slab avalanches are the release of a cohesive layer of snow (a slab) that is generally moist or wet when the flow of liquid water weakens the bond between the slab and the surface below (snow or ground). They often occur during prolonged warming events and/or rain-on-snow events. Wet Slabs can be very unpredictable and destructive.

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.