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Avalanche Forecast

Archived

Dec 24th, 2017–Dec 25th, 2017

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

Regions

Sea To Sky.

Looks like good ol' Saint Nick will be delivering a dusting of new snow for Christmas morning.  Hopefully he will give up the rest of the goods later in the week and spread a bit more of that festive spirit.

Confidence

High - The weather pattern is stable

Weather Forecast

A light dusting (2-5 cm) on new snow is expected late Sunday and early Monday morning.MONDAY: Mix of sun and cloud, light flurries. Accumulation trace. Ridge wind light from the northwest. Temperature -6. Freezing level surface.TUESDAY: Mix of sun and cloud. Ridge wind light from the southwest. Temperature -8. Freezing level surface.WEDNESDAY: Cloudy, flurries. Accumulation trace. Ridge wind light to moderate from the west. Temperature -5. Freezing level surface.

Avalanche Summary

There have been no reports of avalanche activity since Thursday when there was a report of a small (size 1) skier accidental wind slab release on a north aspect in the alpine. On Wednesday, several small, skier-triggered avalanches were reported as well as explosives triggered slab avalanches up to Size 3 on wind-loaded slopes in the alpine and at treeline. See here and here for recent Mountain Information Network (MIN) reports.

Snowpack Summary

The recent storm snow has been redistributed by strong northerly winds scouring windward, north to west aspects and building wind slabs on leeward, south to east aspects in the alpine and exposed treeline areas. This has created a highly variable upper snowpack with areas of both soft snow and hard wind slab, as well as areas of exposed crust depending on aspect and elevation. An average of 20-40cm of settled storm snow now sits on a melt-freeze crust (December 15th layer) that formed on all aspects and elevations. On high north aspects this crust is thin with dry, sugary snow crystals (facets) below. Below the December 15th layer, the late November crust is now buried 70-100 cm with a thin layer of facets above. Beneath this crust the lower snowpack is well settled.

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.