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Avalanche Forecast

Archived

Jan 22nd, 2023–Jan 23rd, 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 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

North Rockies, Sugarbowl, McGregor, Pine Pass.

It's a good time to take a big step back from avalanche terrain. New snow and wind are building fresh wind slabs and adding load to a weak and volatile snowpack. It's uncertain when the tipping point will be reached for large, destructive avalanches to occur and this uncertainty demands a conservative approach and low-consequence terrain selection.

Confidence

Low

Avalanche Summary

Last week, our field team observed several small wind slab avalanches. Check out their latest MIN for more details.

Looking forward to this week, reactive wind slabs are expected to form but concern for large natural and human-triggered deep persistent slab avalanches is at the forefront of our minds. A series of incoming storms will be slowly adding load to a shallow, weak snowpack with multiple layers of concern. It is uncertain when the "tipping point" for large destructive avalanches will be reached but this uncertainty demands conservative and low-consequence terrain selection. Check out this video on incremental loading to learn more.

Please continue to send in your observations through the MIN.

Snowpack Summary

Overnight snowfall has brought 5-15 cm of new snow. The accompanying northwest winds will affect wind-exposed terrain and build fresh wind slabs in lee terrain features. Below the new snow, a sun crust may be found on steep solar aspects.

At lower elevations, a rain crust exists down around 20cm, with reported elevations extending up to 1800 m in the Cariboos and roughly 1200 m in the northern part of the region.

Snowpack depths are shallower than normal, and several buried weak layers have been a concern over the past few weeks. One is a recently buried surface hoar layer found 30 to 60cm deep in sheltered terrain features at treeline and above. At this same depth, a crust exists on steep south-facing slopes. Another layer of facets, crust, and surface hoar was buried around Christmas and is now 50 to 90cm deep. Finally, a layer of large, weak facets buried in November is found near the bottom of the snowpack. This layer is likely most problematic in alpine terrain, where shallower avalanches could scrub down to these basal facets.

Weather Summary

Sunday night

Cloudy with increasing snowfall, 5-10 cm of accumulation. Alpine temperatures drop to a low of -10 C. Ridge wind northwest 40-60 km/h. Freezing level at valley bottom.

Monday

Mainly cloudy with continued snowfall, 5 cm of accumulation. Alpine temperatures rise to -7 C. Ridge wind northwest 45-70 km/h. Freezing level rises to 1100 m.

Tuesday

Cloudy with snowfall, 5-10 cm accumulation. Alpine temperatures reach a high of -6 C. Ridge wind northwest 40-60 km/h. Freezing level rises to 1100 m.

Wednesday

Mainly cloudy with snowfall, 5-15 cm of accumulation. Alpine temperatures reach a high of -1 C. Mostly light westerly ridge wind occasionally gusting to 35 km/h. Freezing level rises to 1400 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.
  • Avoid thin areas like rock outcroppings where you're most likely to trigger avalanches failing on deep weak layers.
  • Uncertainty is best managed through conservative terrain choices at this time.

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.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.