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Avalanche Forecast

Archived

Dec 23rd, 2017–Dec 24th, 2017

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.
Below Treeline
Natural avalanches unlikely.

Regions

Northwest Coastal.

Sheltered terrain not only offers the best riding right now, but also keeps you away from the lingering wind slabs.

Confidence

Moderate - The weather pattern is stable

Weather Forecast

SUNDAY: Sunny with increasing cloud, strong outflow winds, treeline temperatures around -10 C.MONDAY: Clouds clearing throughout the day, moderate northwest winds, treeline temperatures around -12 C.TUESDAY: Sunny, moderate northwest winds, treeline temperatures around -12 C.

Avalanche Summary

No new avalanches have been reported. On Thursday, skiers triggered a few small slabs (size 1) on steep wind-loaded features.

Snowpack Summary

Strong outflow winds have dramatically affected the surface snow, scouring some slopes down to an old crust and forming hard deposits in many other areas. Sheltered areas may still have 20 to 50 cm of powder from previous storms, but winds have come from a variety of directions and affected much of the terrain. Wind slabs may rest on a variety of old surfaces including a thick melt-freeze crust (reported to be 3 to 15 cm thick) and in some sheltered locations soft feathery surface hoar crystals above the crust. The mid-pack is reported to be generally strong below this crust, with the possible exception of areas around Stewart and northern parts of the region where the late October crust can be found deep in the snowpack. This deep crust has been been associated with weak sugary snow and may still be a concern in shallow snowpack areas.

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.