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Avalanche Forecast

Archived

Mar 28th, 2017–Mar 29th, 2017

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

Regions

Cariboos.

If localized snowfall amounts exceed 20 cm the avalanche hazard at treeline is CONSIDERABLE.

Confidence

Moderate - Forecast snowfall amounts are uncertain on Wednesday

Weather Forecast

A series of low pressure systems will sweep across the Interior tonight through tomorrow bringing precipitation and light-moderate winds. A clearing trend with an associated ridge will start to set up later Thursday into Friday. Wednesday: Snow amounts  5-10 cm through the day. Ridgetop winds will be moderate from the West and freezing levels near 1500 m. Thursday: Mostly cloudy with possible sunny breaks. Ridgetop winds light-moderate from the NW. Alpine temperatures near -7 and freezing levels 1500 m. Friday: Mostly cloudy with alpine temperatures high of -2 and freezing levels 1700 m.

Avalanche Summary

On Monday, a natural cornice fall up to size 2 was observed. With continued precipitation and wind, natural avalanche activity may continue. Fragile cornices are also suspect, they are large enough and act as heavy triggers for deeper slab avalanches to release on the slopes below. If you're traveling below treeline where the avalanche hazard is lower than it is in the alpine you should remain diligent with your terrain use, mitigate overhead hazards by avoiding or lingering in run-out zones where large avalanches could come down from above. We remain in a low probability, high consequence scenario for persistent slab avalanches failing on deeply buried weak layers. Check out the recent Forecaster Blogs for more details.

Snowpack Summary

Up to 20 cm of recent storm snow has fallen at upper elevations. This now brings 30-70 cm of accumulated snow over the past week which overlies a rain crust below 2000 m or a sun crust on solar aspects at higher elevations. New wind slabs are developing on leeward slopes and behind terrain features and large, fragile cornices exist along ridgelines. At lower elevations, there may be multiple crust layers in the upper snowpack which are now generally bonded. At higher elevations, the February weak layers are down 120-150 cm and woke up during last week's storm with many avalanches stepping down to them. The deep mid-December facet layer and November rain crust both still linger near the bottom of the snowpack and a few avalanches and cornice falls have also stepped down to these layers last week resulting in some very large full depth avalanches.

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.

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.