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Avalanche Forecast

Archived

Jan 16th, 2023–Jan 17th, 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 Columbia, South Columbia, Blue River, Clearwater, Premier, Grohman, Clemina, Jordan, North Monashee, North Selkirk, Shuswap, West Purcell, Badshot-Battle, Central Selkirk, Goat, Gold, Kokanee, North Okanagan, Retallack, Valhalla, Whatshan.

Continue to make conservative terrain choices and consider the consequences of an avalanche on a chosen slope. There is variability in the snowpack throughout the region, but what is consistent is that the snowpack is shallower and weaker than average.

Confidence

High

Avalanche Summary

A widespread avalanche cycle occurred during the storm on Friday and Saturday, producing large avalanches at all elevations and aspects on multiple persistent weak layers. Most of the activity was on the two surface hoar layers from January, but there was also activity on the November facets near the bottom of the snowpack. Avalanches ranged in size from 1.5 to 3.5.

Human triggered avalanche activity continued on Sunday, with numerous reports of remote, accidental, and controlled avalanches. These avalanches were generally up to size 2 and were triggered on one of the two surface hoar layers buried in January.

Looking forward, there may be a slight decline in the reactivity of these weak layers, but the snowpack is inherently weak and large human triggered avalanches remain likely.

Snowpack Summary

A recent layer of surface hoar and a crust on south facing slopes can be found under 20 to 60 cm of new dense storm snow at treeline and above. Wind slabs exist on north, west, and east facing terrain at treeline and above. A surface crust will form below 1800 m as the freezing level drops.

There are four additional weak layers in the snowpack. The most reactive in recent days have been the layer mentioned above and another surface hoar layer from early January. The bottom of the snowpack is made up of large facets buried in late November. This layer remains a concern.

In general, this year's snowpack is complicated, weak, and shallow. Keep this in mind as you move through the mountains.

Weather Summary

Monday night

Cloudy with flurries bringing trace amounts of snow, 20 km/h southwest wind, freezing level drops to valley bottom with treeline temperatures cooling to -7 °C.

Tuesday

Mostly cloudy with the possibility of light flurries bringing trace amounts of snow, 20 km/h southwest wind, freezing level around 1000 m with treeline temperatures around -5 °C.

Wednesday

Mostly cloudy with light flurries bringing trace amounts of snow, 20 to 40 km/h southwest wind, treeline temperatures around -6 °C.

Thursday

Cloudy with scattered flurries bringing 5 to 10 cm of snow, 40 km/h southwest wind, treeline temperatures around -6 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Be mindful that deep instabilities are still present and have produced recent large avalanches.
  • Carefully assess open slopes and convex rolls where buried surface hoar may be preserved.
  • 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

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.

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.