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Avalanche Forecast

Archived

Dec 13th, 2022–Dec 14th, 2022

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

Regions

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

Fresh wind slabs are expected to form throughout the day as northwesterly winds redistribute the surface snow into lee areas in the alpine and treeline.

Concern for buried weak layers continues to demand conservative terrain selection and good travel habits.

Confidence

Moderate

Avalanche Summary

During the storm on Friday, a natural avalanche cycle occurred, with storm slab avalanches up to size 2 observed in the alpine and treeline. Numerous skier-triggered storm slabs were reported in this time period as well. Notably, some explosive control produced persistent slab avalanches that failed on the mid-Nov crust down about 50cm and propagated around 50m wide.

Over the weekend, natural activity began to taper but human triggering remained likely! Many riders in the Squamish and Whistler area got surprised by size 1-2 slab avalanches. These slabs mainly occurred on wind-loaded slopes on north and west aspects in the alpine and treeline. Check out these MIN reports for examples (MIN1) (MIN2).

Looking forward to Wednesday, we expect fresh, reactive wind slabs to form as northwest winds redistribute the surface snow into lee areas. Keep in mind that small avalanches have the potential to 'step down' to deeply buried weak layers resulting in larger than expected avalanches.

Thank you for sharing your observations over the weekend! Please keep posting to the MIN; it helps strengthen our information gathering.

Snowpack Summary

Surface: Large surface hoar growth has been observed in sheltered areas. Around 30 to 50 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 of storm snow accumulations.Upper-pack: The upper snowpack consists of 20-50 cm of light but settling snow. 50 cm down large surface hoar (up to 10 mm) has been observed mainly in shaded or sheltered areas. Mid-pack: 40-150 cm down is a late November crust, with soft facets above. This is likely the critical snowpack weakness. Professionals are concerned about the possibility of avalanches releasing at this deeper interface with the new snow load and warm temperatures.

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

Tuesday night

Clear periods. Alpine temperatures drop to a low of -5 °C. Ridge wind light to 25 km/h from the northwest. Freezing level at valley bottom.

Wednesday

Sunny with cloudy periods. Alpine temperatures reach a high of -2 °C. Ridge wind 25km/h gusting to 40 km/h. Freezing level at valley bottom.

Thursday

Sunny with cloudy periods. Alpine temperatures reach a high of 2 °C. Ridge wind 30 km/h gusting to 55 km/h. Freezing level rises to 1900 metres.

Friday

Sunny. Alpine temperatures reach a high of 3 °C. Mostly light ridge wind occasionally gusting to 45 km/h. Freezing level rises to 2100 metres.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • 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.
  • Approach steep open slopes at and below treeline cautiously, buried surface hoar may exist.
  • Be aware of the potential for surprisingly large avalanches due to deeply buried weak layers.

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.