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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

Cariboos.

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 early 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 early morning hours and isolated flurries, trace of new snow and rain up to treeline, moderate northerly wind, alpine low +1 C, freezing level around 2800 m and dropping to 1700 m in the early morning hours.

Sunday: Clouds with isolated flurries in the morning and sunny from mid-morning onward, trace of new snow and rain below treeline, moderate to strong northeast wind, alpine high 0 C, freezing level 1700 m.

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

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

Avalanche Summary

A widespread wet loose avalanche cycle to size 3 and several cornice failures entraining snow on the slopes below were observed on Friday and Thursday (see this MIN). Increased wet loose and potentially wet slab avalanche activity and cornice failures likely continued on Saturday. 

Several cornices failed recently. Most did not trigger slabs on slopes below except for a few that triggered size 2 slabs on extreme north facing alpine slopes. 

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. 20-40 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. Many natural cornice falls were observed recently. Some triggered slabs on the slopes below.

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 triggering buried weak layers increases. 

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.
  • The likelihood of deep persistent slab avalanches will increase with each day of warm weather.

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.