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Avalanche Forecast

Archived

Dec 19th, 2013–Dec 20th, 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 possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

Cariboos.

Forecasters are operating with limited field data at this time. If you've been in the backcountry we'd love to hear what you're seeing. Please send observations to: [email protected]

Confidence

Fair

Weather Forecast

Synopsis: Upper NW flow brings significant precipitation to the North Coast over the next few days. A small amount of snow will make it to the Cariboos accompanied by variable winds.Friday: Freezing Level: Valley Bottom; Precip: 2/4mm 4/8cm Wind: Light NWSaturday: Freezing Level: Valley Bottom; Precip: Trace Wind: Lht gusting Strong, NWSunday: Freezing Level: 800m Precip: Trace; Wind: Light SW

Avalanche Summary

A small wind slab avalanche cycle to size 2 was reported Wednesday.

Snowpack Summary

Snowpack depths vary widely with reports of up to 180cm at tree line in some parts of the region. The upper snowpack contains storm snow, wind slabs, surface hoar, and facets. Previously warm temps and as much as 70cm of new snow have combined to form a cohesive slab on top of the surface hoar and facets. It's difficult to determine if the slab is currently reactive to light triggers like skiers and sledders. Deeper in the mid-pack a couple of persistent weak layers (surface hoar and facets) can be found that formed in mid and late November. Near the base of the snowpack an early season rain crust exists.

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.

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.