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Avalanche Forecast

Archived

Feb 14th, 2021–Feb 15th, 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

South Columbia.

Watch for wind slabs in unusual places as winds have varied in direction. Given recent cold weather, 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

SUNDAY NIGHT: Cloudy, isolated flurries with trace accumulations, light south wind, alpine temperatures around -12 C.

MONDAY: Mainly cloudy, isolated flurries with trace accumulations, light south wind, alpine temperatures around -12 C. 

TUESDAY: Cloudy, light west winds with moderate gusts at ridgetop, isolated flurries with trace accumulations, alpine temperatures around -11 C.

WEDNESDAY: Cloudy, light west winds with moderate gusts at ridgetop, isolated flurries with trace accumulations, alpine temperatures around -11 C.

Avalanche Summary

Over the weekend, numerous small to large (up to size 2) natural and human-triggered wind slab avalanches were reported across a wide range of aspects above 2100 m that broke 10-40 cm deep. These MIN reports, both from Mt. Brennan on Saturday (here and here), offer helpful examples of this avalanche activity. There continue to be reports of small (size 1-1.5) dry loose avalanches. 

Observations of avalanches on the late January persistent weak layer continue to trickle in. This MIN report from Joss Mountain on Friday shows that the surface hoar remains reactive on lower elevation cutblock features. Last week, a wind slab on a southeast aspect was thought to step-down to the late January crust/facet interface to produce a size 3 avalanche on London Ridge, and there was a size 1.5 skier triggered slab near Revelstoke (MIN report).

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 is becoming soft and faceted with the cold temperatures. 60-120 cm of snow from February is settling over a weak layer of surface hoar that has shown reactivity at treeline or in "treeline-like" features, like cutblocks, below treeline. On steep south-facing terrain, this layer may consist of facets on a sun crust. This persistent weak layer will be slow to gain strength and requires careful terrain selection. 

The mid/lower snowpack is generally strong and settled in most areas.

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 a persistent slab.
  • 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.