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Avalanche Forecast

Archived

Feb 7th, 2013–Feb 8th, 2013

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 unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

Cariboos.

Weak layers within the upper snowpack have yet to be tested by the effects of the sun. Blue skies and fresh snow may tempt you into steeper and bigger terrain. Maintain a diligent approach to terrain selection to best manage the current conditions.

Confidence

Fair - Timing or intensity of solar radiation is uncertain for the entire period

Weather Forecast

Friday: A weakening upper trough moves out of the region as a ridge of high pressure makes its way in. The initial changes in the weather pattern will bring only trace amounts of new snow and broken cloud. Periods of sunshine and solar radiation may exist. Ridgetop winds will be light-moderate from the NW. Treeline temperatures will be near -5 and freezing levels around 900 m. Saturday: The ridge of high pressure builds and brings dry conditions with periods of scattered to few clouds allowing some sunny alpine skies. Ridgetop winds will blow light-moderate from the NW. Treeline temperatures near -2 and freezing levels rising to 1300 m then dropping to valley bottom overnight.Sunday: The upper ridge strengthens with continued dryer conditions. Ridgetop winds light from the NW. Treeline temperatures near -5 and freezing levels around 1100 m.

Avalanche Summary

Some natural avalanche activity occurred on Wednesday. One loose dry avalanche size 2.5 initiated from steep East facing terrain above 2000 m and a skier triggered size 1 slab avalanche from a NW aspect around 1900 m.  Earlier this week a large natural size 3 slab avalanche was reported from a large uneven south facing slope, the suspected failure plane being the buried crust down 40-80 cm. Heads up out there! I suspect avalanche activity to continue through the forecast period, additional concerns being periods of solar radiation as a natural trigger.

Snowpack Summary

20-40 cm of new snow sits on wind slabs and recently buried surface hoar, sun crusts and facets that formed at the beginning of February. Old storm snow has settled into a dense slab that could be triggered by skiers or sledders and produce avalanches up to size 2.0. This slab sits on a persistent weak interface deeper (40-80 cm down) in the snowpack, comprising yet again of crusts, surface hoar and facets that were buried January 23rd. Use extra caution on large open slopes, cutblocks and convex rolls at and below treeline where buried surface hoar may be preserved. Wind slabs continue to develop and stiffen on lee slopes (N-SE) and behind terrain features like ridgelines and ribs.The midpack is generally well settled and strong. Average snowpack depth at treeline elevations is near 200 cm.

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.

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.