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Avalanche Forecast

Archived

Feb 8th, 2020–Feb 9th, 2020

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.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Kootenay Boundary.

Enjoy glimpses of the sun! Wind direction shifted from southwest to northwest and back again. Watch out for wind slabs on all aspects when transitioning into wind affected terrain. 

Confidence

High -

Weather Forecast

Saturday Night: Flurries, accumulation up to 5 cm, light northerly wind, alpine high -6 C, freezing level at valley bottom.

Sunday: Mix of sun and cloud, moderate northwest wind, alpine high -8 C, freezing level 800 m.

Monday: Mostly sunny, light to moderate northerly wind, alpine high -9 C, freezing level 900 m.

Tuesday: Mix of sun and cloud, light southwest wind, alpine high -6 C, freezing level 900 m.

Avalanche Summary

On Friday a few small (size 1) slab avalanches were triggered by skiers in lee terrain features. 

On Thursday a few large (size 2-2.5) slab avalanches released naturally during the night. One large (size 3) slab avalanche was triggered by explosives in the west of the region. Several small (size 1-1.5) slab avalanches were triggered by skiers mainly on south and east aspects. 

On Wednesday several small (size 1) slab avalanches in the alpine were triggered by skiers. Several small (size 1) natural and skier triggered loose dry avalanches were reported in steep terrain at treeline and in the alpine. 

Snowpack Summary

Wind switching directions has redistributed recent new snow onto a variety of aspects. The snow surface varies from low density in wind sheltered areas to wind slab. Specific terrain features at treeline and in the alpine were scoured to a crust from early February before this last storm hit the region. As high as 2000 m, the upper snowpack contains a crust from recent warming and rain events. Generally the recent storm snow seems to bond well with the crust below. Several avalanches were observed to release within the recent storm snow. However, some avalanches slid on the crust below. 

Weak facet/crust layers near the base of the snowpack are particularly noteworthy in the western Boundary area.

Terrain and Travel

  • Recent wind has varied in direction so watch for wind slabs on all aspects.
  • Carefully evaluate steep lines for wind slabs.
  • A moist or wet snow surface, pinwheeling and natural avalanches are all indicators of a weakening snowpack.

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.