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Avalanche Forecast

Archived

Apr 16th, 2021–Apr 17th, 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.

With multiple warm days in a row and high overnight freezing levels it is important to start and finish your day early. Look for north facing objectives without overhead cornices. Plan your egress route carefully.

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

Confidence

High - We are confident the likelihood of avalanche will increase with the arrival of the forecast weather.

Weather Forecast

A ridge of high pressure continues to bring sunny and dry weather with freezing levels around 3000 m even at night. On Sunday the ridge is forecast to break down bringing light precipitation and lowering freezing levels.

Friday night: Clear, light north wind, alpine low +4 C, freezing level 3000 m. 

Saturday: Sunny, light to moderate northwest wind, alpine high +8 C, freezing level 2900 m.

Sunday: Mix of sun and cloud with isolated flurries, up to 3 cm new snow and rain below treeline, moderate to strong northeast wind, alpine high +2 C, freezing level lowering to 1700 m.

Monday: Sunny, light to moderate northeast wind, alpine high +5 C, freezing level 2100 m

Avalanche Summary

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

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. 

A couple of natural cornice failures size 2.5 observed last Sunday did not trigger slabs on slopes below. 

Snowpack Summary

The snow surface consists of a melt-freeze crust on solar aspects and shaded aspects up to treeline which transitions into moist/wet snow during the day. Dry snow might still be found on northerly aspects high in the alpine. 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. 

Previous 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. However, with each day of warm weather the likelihood of persistent slab avalanches increases slightly. 

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.