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Avalanche Forecast

Archived

Dec 26th, 2017–Dec 27th, 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

Northwest Inland.

Cold conditions persist. If you get out in the mountains this week please share your photos and observations on the Mountain Information Network (MIN)!

Confidence

High - The weather pattern is stable

Weather Forecast

WEDNESDAY: Mostly sunny, light winds, treeline temperatures around -18 C.THURSDAY: Mix of sun and cloud, light winds, treeline temperatures around -18 C.FRIDAY: Mix of sun and cloud, light winds, treeline temperatures around -18 C.

Avalanche Summary

A few small natural wind slabs were reported in steep south facing terrain west of Smithers on the weekend. Wind slabs showed some reactivity to human triggers last week, but cold temperatures have generally made them difficult to trigger.

Snowpack Summary

Surface snow has been affected by winds from a variety of directions. The degree of wind effect varies throughout the region, with the most dramatic winds associated with outflow conditions in the western parts of the region near coastal inlets. Sheltered areas may still have 10-30 cm of powder from previous storms. A variable weak layer can be found roughly 20 cm below the surface, but in most places insufficient snow has fallen for it to be reactive. The layer comprises of crusts on solar aspects and feathery surface hoar crystals in sheltered locations.The lower snowpack is generally well settled with two prominent crusts. The late November crust can be found 30-50 cm below the surface and the October crust is near the base of the 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.