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Avalanche Forecast

Archived

Dec 10th, 2022–Dec 11th, 2022

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

Regions

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

The snowpack is thin, weak, and won't gain strength after a storm like it usually does. Stay conservative as you hunt for powder!

 

Confidence

Moderate

Avalanche Summary

Around the Whistler area on Friday size 1 to 2 soft storm slab avalanches were triggered with explosives, by skiers, and naturally. Interestingly, some explosives released size 2 on the mid-Nov crust down about 50cm and propagated around 50m wide.

Please keep sharing your observations via the MIN; it helps strengthen our information gathering!

Snowpack Summary

Surface: Around 20 to 30 cm of recent snow, but also at or near the surface you can find wind scoured, wind pressed, and of course wind slabs. In wind sheltered deep snow areas there could be as much as 70 cm storm snow accumulations.Upper-pack: on shaded terrain at all elevations large surface hoar (up to 10 mm) and generally unconsolidated snow. The upper snowpack consists of 20-50 cm of light but settling snow.Mid-pack: 50 cm down (maybe 70 to 100 cm in deep wind loaded areas) is a late November crust, with soft facets above. This is likely the critical snowpack weakness. Professionals are concerned about the possibility avalanches releasing at this deeper interface with the new snow load. So is Sofia (thanks for the MIN); I especially like her snowprofile photo!

Total snow depths remain low for early December with 90 to 140 cm at treeline and up to 200 cm in the alpine. Much of the below treeline elevation band is below the threshold for avalanches.

Weather Summary

Saturday NightStorm ends with only a trace to a few cm of snow overnight. Temps staying warm between -5 and 0 near treeline with freezing level around 800 m. Southeast to south wind moderate but diminishing overnight.

SundayDry with only a trace of snow possible. Continued warm with temperatures a few degrees below zero near treeline. Freezing level steady around 700 m. Light westerly wind. Mix of sun and cloud depending on location.

Monday

Dry. Cooler with temps between -5 to -10 C and freezing level to valley bottom. Northerly light wind with outflow from the interior through the passes and in the major valleys. Mix of sun and cloud clearing in the afternoon.

Tuesday

Similar to Monday but more sun and less cloud.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • The best and safest riding will be on slopes that have soft snow without any slab properties.
  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • If triggered, wind slabs avalanches may step down to deeper layers resulting in larger avalanches.
  • Use caution above cliffs and terrain traps where even small avalanches may have severe consequences.

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.