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Avalanche Forecast

Archived

Dec 3rd, 2013–Dec 4th, 2013

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

South Columbia.

Confidence

Fair - Wind effect is extremely variable

Weather Forecast

Cold and mostly clear skies are expected for the forecast period as a dry arctic air mass becomes firmly embedded over British Columbia. Ridgetop temperatures are expected to hover around -16 on Wednesday and Thursday, and then drop to about -20 on Friday. Expect periods of moderate north/northeasterly winds.

Avalanche Summary

On Monday a size 3 natural slab avalanche was noted in the southwest corner of the region. It occurred on a north/northeast aspect at 2400m. The exact interface is unknown. In the same corner of the region a size 2.5 slab avalanche was observed releasing on a south facing slope at about 2100m on the recently buried sun crust. In the northwest of the region, fairly widespread natural slab activity to size 2 was also noted. The most recently buried surface hoar interface was the suspect in these events. On Tuesday, numerous size 2 natural wind and storm slab avalanches were observed in Glacier National Park along the highway corridor. I would expect similar conditions throughout the South Columbia Region.

Snowpack Summary

A potent storm slab now exists throughout the region and is ripe for rider triggering at all elevation bands. In deeper snowpack areas this new slab is about 60cm deep and covers a complex variety of old surfaces which include melt-freeze crusts on previously sun-exposed slopes and touchy surface hoar crystals in sheltered terrain. These weaknesses are likely to persist for some time with potential for large and destructive avalanches. To add to the complexity of the current scenario, east/northeasterly winds are responsible for new windslabs on south and west facing terrain.In the mid snowpack you may find a layer of surface hoar or a crust buried in mid-November which sits about 60cm above the ground. Near the base of the snowpack you'll find the October crust/facet combo. The most likely place you'd trigger this layer is on smooth, planar, high north facing slopes, especially if the snowpack is unusually shallow in that area.These persistent layers are slowly becoming more difficult to trigger. However, they have the potential to cause very large and destructive avalanches, and may 'wake-up' with the increased load of the new snow.

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.

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.