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Avalanche Forecast

Archived

Feb 15th, 2021–Feb 16th, 2021

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

Cariboos.

Watch for wind slabs in unusual places. These slabs have potential to break wider than expected and may be slow to bond. Read about managing these conditions in this forecaster blog. 

Confidence

Moderate - Confidence is due to a stable weather pattern with little change expected.

Weather Forecast

MONDAY NIGHT: Mostly cloudy, light flurries with a trace of snow, moderate west wind at ridgetop, alpine temperatures around -13 C. 

TUESDAY: Cloudy, light flurries with a trace of snow, moderate west wind with strong gusts at ridgetop, alpine temperatures around -13 C.  

WEDNESDAY: Cloudy, light flurries with a trace of snow, moderate southwest wind, alpine temperatures around -12 C. 

THURSDAY: Increasing cloud, strong south winds, alpine high temperatures around -8 C. 

Avalanche Summary

On Saturday, observers near Valemount reported small loose dry sluffs on steep terrain in the trees (MIN report).

On Thursday, a MIN report in the south of the region detailed a spike in wind speed and a shift in direction to northeast that formed touchy slabs, loaded cornices to their breaking point, and likely initiated a large avalanche in the alpine. A MIN report on Saturday indicated that a similar pattern of wind slab and cornice activity had previously occurred in areas around Valemount . 

Earlier in February, there was widespread avalanche activity on a weak layer of buried surface hoar, mostly on treeline features (see some photos in the MIN reports here, here, and here). 

Snowpack Summary

Winds have varied in strength and direction over the past week, loading cornices and forming wind slabs at upper elevations that may still be possible to trigger. Watch for these wind slabs in unusual places as complicated cross-loading and reverse-loading patterns are prevalent. Wind slabs may overlie weak, sugary, faceted snow, meaning that they could break wider than expected and will likely be slow to bond. 

In wind-sheltered areas, the upper snowpack has become soft and faceted from the cold temperatures. 40-70 cm of snow from February is settling over a reactive weak layer of surface hoar buried in late January. Reactivity on this layer has primarily been observed at treeline and in "treeline-like" features, like cutblocks, that are below treeline. Snowpack test results continue to show instability on this layer, like this MIN report from Allan Creek on Friday. On steep south-facing terrain, this layer may consist of facets on a sun crust.  

Additional weak layers may present in the lower snowpack, but are not a concern in most areas until we see significant snow loading or rapid warming. 

Terrain and Travel

  • Recent wind has varied in direction so watch for wind slabs on all aspects.
  • Approach lee and cross-loaded slopes with caution.
  • Be aware of the potential for large avalanches due to the presence of buried surface hoar.
  • Extra caution is needed around cornices under the current conditions.

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.