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Avalanche Forecast

Archived

Apr 5th, 2021–Apr 6th, 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, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.

Regions

Cariboos.

Periods of sunshine can pack a punch and trigger natural avalanches and cornice fall. Give cornices a wide berth from above and below. 

Pockets of wind slab may exist on leeward features in the alpine and could be triggered by the weight of a person. 

Confidence

High -

Weather Forecast

The region will start to see the effects of the next frontal system by late Tuesday. This will bring moderate snow amounts accompanied by strong southwest wind.

Tuesday: Mix of sun and cloud with light snow up 5-10 cm. Ridgetop wind strong from the southwest. Alpine temperatures near -6 and freezing levels 1700 m. 

Wednesday: Snow 10-20 cm. Ridgetop wind moderate to strong from the southwest. Alpine temperatures -7 and freezing levels 1400 m. 

Thursday: Mix of sun and cloud with a trace of new snow. Ridgetop wind light from the southwest. Alpine temperatures near -7 and freezing lvels 1300 m. 

Avalanche Summary

On Monday, reports from our Field team in the Dore river area noted evidence of loose-wet avalanches up to size 2 and some cornice falls. One larger slab avalanche (several days old) size 2.5 was also seen on a steep East aspect in the alpine. 

Reports from Sunday noted that the recent snow (10-20 cm) was sluffing from steep terrain features and loose-wet avalanches were seen up to size 1 from solar aspects below 1800 m. The recent snow from Sundays' storm seems to be bonding to previous snow surfaces. 

Cloud cover, a bit of new snow, and strong southwest wind are expected to keep snow surfaces cool on Tuesday. Natural avalanche activity may taper. However; things can change rapidly and if the sun shines, natural avalanche activity and cornice failures may spike. 

We regret to report a fatality on Eureka Peak, east of Williams Lake on March 29. A human-triggered cornice failure resulted in a size 2.5 slab avalanche. It is important to remember to stay well back from ridgetops that might be corniced and to avoid slopes with overhead cornice exposure especially under the current conditions where recent rapid growth has made them large and fragile.

Snowpack Summary

10-20 cm of recent snow accompanied by strong southwest wind may have formed wind slabs on leeward slopes at upper elevations. Reports indicate that this recent snow is bonding to a variety of underlying surfaces which include wind-affected snow in the alpine, crust on solar aspects, and below 1900 m. Below this elevation and on solar aspects the new snow dusts crusty surfaces down to 1500 m. Below 1500 m, the moist snowpack is quickly diminishing.

Recent warm weather is 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

  • Avoid slopes when the solar radiation is strong, especially if they have large cornices overhead.
  • Be careful with wind slabs, especially in steep, unsupported and/or convex terrain features.
  • Use ridges or ribs to avoid areas of wind loaded snow.
  • Pay attention to cornices and give them a wide berth when traveling on or below ridges.

Problems

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.

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.