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Avalanche Forecast

Archived

Feb 19th, 2023–Feb 20th, 2023

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

Regions

Sea To Sky, Brandywine, Garibaldi, Homathko, Powell River, Spearhead, Tantalus, Sasquatch.

A period of snowfall and strong winds are expected over the coming 48-hour period.

Avalanche danger ratings are certain to rise, expect to encounter increasingly sensitive wind slabs as sustained strong winds will continue to add more mass to an already established avalanche problem.

Seek well support low angle terrain that avoids steep lee aspect wind-loaded areas.

Carefully evaluate wind loading as you move through terrain and investigate the bond of wind slabs to the crust below.

Confidence

Moderate

Avalanche Summary

On Saturday, numerous reports of both skier and explosive trigger small (size 1-1.5) windslabs avalanches, similarities with the reported avalanches are they failed in the lee of prevailing winds on convex roll features.

Reports of a very large (size 3) avalanche that has impacted a snowmobile access road near Brandywine. No human involvement, however very few details are currently available. Photos can be viewed at this link

On Friday, explosive control and ski cutting produced small (size 1) avalanches on lee aspects (north) terrain. Noted observations included mid-afternoon small (size 1) dry loose avalanche activity, that initiated out of very steep and thin rocky terrain.

On Thursday, ski-cutting activity produced numerous small (size 1) dry loose avalanches, these were found on steep terrain with some operators describing them as "power sluffs".

On Tuesday, A snowmobiler remote triggered a size 2 persistent avalanche in the Callaghan. The avalanche was reported to be triggered from 10 m away and was adjacent to a heavy traffic area. We suspect this avalanche slid on the mid-January persistent weak layer. See the MIN for details and photos. This is the latest human-triggered avalanche on this persistent weak layer in the region.

For more evidence of this weak layer see this MIN report from last Wednesday when a rider at Chocolate Bowl triggered a size 2.5 persistent avalanche. Find another example in this MIN from a skier accidental size 2 persistent slab avalanche that occurred on Saturday.

On Monday afternoon, search and rescue technicians responded to a fatal avalanche incident north of the Sea to Sky region. The avalanche is believed to have occurred on Saturday and was initiated in a shallow rocky area. See the MIN for more details.

Snowpack Summary

Currently, available snow amounts of between 15 and 25 cm are being redistributed via moderate variable winds over a variety of surfaces including facets, old wind slabs, and a thin breakable crust below 1650 m. In sheltered areas above 1200 m snow remains dry and unconsolidated.

Expected north through to west winds with velocities between 60 and 80 km/h are likely to strip and press north-facing terrain. New snow and available snow for transport will begin to deposit on south through to east aspects slopes and terrain features.

Two concerning crusts are found in the mid-pack at varying depths and are widespread throughout the region. A crust from late January is found at all elevations down 40-100 cm with small facets above it. In the Rhododendron and Pemberton Icefield area, this crust has been reactive to rider traffic and in test pits at treeline. In the Brandywine area, a crust found 80-200 cm deep resulted in a few surprisingly large rider-triggered avalanches last week. This layer exists to 1900 m in these areas.

Total snowpack depths are approaching 300 cm in some areas.

Weather Summary

Sunday Night

Cloudy with light snowfall, 1 to 5 cm accumulation. Winds northwest 70 km/h gusting 90 km/h. Treeline temperature -3 °C. Freezing level 1000 m.

Monday

Cloudy with moderate to heavy snowfall beginning late in the afternoon, 10 to 20 cm accumulation. Winds northwest 40 km/h. Treeline temperature -3 °C. Freezing level 1000 m.

Tuesday

Cloudy with very isolated light flurries, trace amounts of accumulation. Winds northwest 40 km/h easing to 20 km/h. Treeline temperature -8 °C. Freezing level descending to 400 m mid-day.

Wednesday

Clearing with no precipitation forecast. Winds southeast 10 km/h . Treeline temperature -9 °C. Freezing level descending to 0 m mid-day.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Fresh wind slabs will likely form throughout the day, diligently watch for changing conditions.
  • Avoid steep, rocky, and wind effected areas where triggering slabs is more likely.
  • Potential for wide propagation exists, fresh slabs may rest on surface hoar, facets and/or crust.
  • Be alert to conditions that change throughout the day.

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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.