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Avalanche Forecast

Archived

Feb 2nd, 2018–Feb 3rd, 2018

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

Regions

Cariboos.

Intense snowfall and strong wind will almost certainly initiate a very large and destructive natural avalanche cycle on Saturday. Only the most simple avalanche terrain free of overhead hazard is appropriate at this time.

Confidence

Moderate - Forecast snowfall amounts are uncertain on Saturday

Weather Forecast

The provincial weather pattern features a clash of titans as juicy warm air streams into the northern interior and then smashes into a rather bullish Arctic front. The Cariboos and North Columbias are expected to see the most action from this engagement, strong snow and wind are expected through Friday night before a brief drying trend takes hold Saturday. We know that weather models do not capture these kinds of events well, there could be more snow and wind than forecast, and there is increased potential for very heavy snowfall locally. Take the following ranges as a suggestion, but don't bet the house on them.(FRIDAY: 15 to 30 cm, strong west wind)FRIDAY NIGHT: Freezing level around 1300 m, strong west/northwest wind, 20 to 40 cm of snow. SATURDAY: Overcast initially, clearing throughout the day, freezing level at valley bottom, strong northwest wind, 1 to 5 cm of snow possible in the morning.SUNDAY: Overcast, freezing level at valley bottom, light to moderate west/southwest wind, 5 to 10 cm of snow possible.

Avalanche Summary

On Thursday explosive control work produced avalanches to size 2.5 failing on both the mid and early January interfaces. These avalanches ran on north, northeast, east and southeast facing features between 1600 and 2600 m. A cornice failure resulted in a size 2 wind slab avalanche on a steep north facing terrain feature at 2100 m. Reports from Wednesday included more observations of widespread natural activity that took place over the previous few days. Numerous recent size 2-3 releases were observed on all aspects at all elevations and several avalanches reached size 4. Subsequent explosives control yielded storm slab and wind slab releases from size 2-2.5 and persistent slab results generally from size 2.5-3. The early January persistent weak layer was named as the primary failure plane for persistent slab releases, although several larger releases stepped down to the mid-December layer.On Tuesday natural avalanches to size 2.5 were reported on northwest facing slopes at 2200 m, running on the early January interface. A size 2.5 avalanche on a northeast facing slope at 1920 m resulted in a single fatality in Clemina Creek. More details available here.

Snowpack Summary

25-50 cm of storm snow fell between Sunday and Tuesday night. Temperatures reached -2 C at treeline in the south of the region (and +2 C near Barkerville) on Monday afternoon. The new snow sits on an unstable snowpack with three active weak layers we are monitoring:1) Down about 40-80 cm is a crust and/or surface hoar layer that was buried in mid-January. The surface hoar is up to 10 mm in size, found at all elevation bands and has been very reactive on north through east aspects between 1900-2600 m. 2) Deeper in the snowpack, the early-January persistent weak layer is found 50 to 100 cm below the surface. This layer has been reported as the most active persistent weak layer during a recent natural avalanche cycle that took place in the region. It has also been the most reactive to recent explosives control.3) Another weak layer buried mid-December consisting of a facet/surface hoar/crust combination is buried 100 to 150 cm deep. It has been most problematic at and below tree line. Many avalanches that failed at shallower weak layers 'stepped down' to this interface during the recent avalanche cycle and in recent explosives control.See here for some recent snowpack test results.

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.

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.