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Avalanche Forecast

Archived

Feb 5th, 2018–Feb 6th, 2018

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

Regions

South Coast Inland.

New snow totals are uncertain in this weather pattern. Wind slabs and cornices are reactive to human triggers: Give both a wide berth and avoid overhead hazard.

Confidence

Low - Intensity of incoming weather systems is uncertain

Weather Forecast

Tuesday: Cloudy with flurries (10cm snow in the south and 5 cm in the north) / Moderate west winds / Freezing level near 1100m.Wednesday: 5-20 cm of snow above 1500m in the south and up to 5-10 cm possible in the north / Moderate to strong southwest winds / Freezing level rising to 2000m in the afternoon. Thursday: 5-20 cm snow above 1000m in the south and 0-5 cm in the north / Light to moderate westerly winds / Freezing level at 1300mNote: Forecast precipitation amounts are uncertain in the south (Coquihalla) for the Wednesday-Thursday storm.

Avalanche Summary

On Saturday in the north of the region, skiers triggered a size 2 wind slab avalanche on a north east facing slope near 2050m. See the MIN report for more information.Also on Saturday in the Duffey zone, we had reports of a cornice-triggered size 3 wind slab on a north east facing slope near 2100m. See the MIN report for more information. On Wednesday in the Duffey area, explosives control triggered a size 2.5 and 2 size 3 persistent slab avalanches in north-facing alpine terrain. The early January crust was the culprit in all 3 of these avalanches. More alarming was a skier-triggered size 3 slab avalanche in the Birkenhead Lake area on the same day. The avalanche was triggered on a northwest facing slope at 2200m, was about 120cm deep and ran a distance of approximately 400m. Nobody was injured in the event. These avalanches demonstrate that you may be dealing with more than just the most recent storm snow in this part of the region.

Snowpack Summary

Recent snowfall totals are highly variable. In the south, up to 40cm of snow fell in the alpine over the past two days, while tree line elevations saw 10-20cm and temperatures near 0 degrees on Monday afternoon. In the north, new snow totals were 15-20cm in the alpine, and rapidly decreasing below 1800m.In the alpine, winds were moderate to strong from the south / east (Coquihalla) and moderate from the south / west (Duffey zone), creating fresh wind slabs in exposed down wind (lee) terrain. At lower treeline and below, warm temperatures (and rain in many locations) have created heavy snow and tough riding conditions. The new snow adds to the 80-150cm of snow that fell during the last few weeks of January. These series of storms were accompanied by strong to extreme winds which resulted in extensive scouring and impressive cornice growth in upper elevation terrain. These accumulations sit on crusts from early and mid-January which generally show signs of bonding to the overlying snow; however, they been sensitive to skier triggering in at last one recent avalanche in the north of the region (see Avalanche Activity Discussion for details).

Problems

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.