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Avalanche Forecast

Archived

Jan 30th, 2016–Jan 31st, 2016

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

Regions

Cariboos.

A recently formed storm slab and touchy persistent weak layers are making for tricky conditions. Conservative terrain selection is critical.In the North Rockies, conditions are also tricky. Check out the new blog at http://goo.gl/j4awOS or click here

Confidence

Moderate - Timing or intensity of solar radiation is uncertain

Weather Forecast

A mix of sun and cloud is expected for Sunday with light intermittent flurries possible. Freezing levels are expected to fall to valley bottom overnight and climb to around 800m on Sunday afternoon. Alpine winds are forecast to be light from the northwest. Light snowfall is forecast for Monday but less than 5cm is expected. Freezing levels are expected to reach around 1000m on Monday and alpine winds are forecast to be moderate from the west to northwest. Similar conditions are expected for Tuesday with light snowfall, cool temperatures, and moderate west winds.

Avalanche Summary

On Friday, numerous natural avalanches up to size 2.5 were reported in the region. Many of these avalanches were reported to have started in steep unskiable terrain or big faces and were typically starting as dry slabs and entraining moist snow below 1700-1800m. Three skier triggered avalanches were also reported. One was remotely triggered from 10m away on an east aspect at 2000m. This released down 70cm suggesting it failed on the early January surface hoar layer. A size 1.5 was reported on a west aspect at 1900m failing down 100cm on the early January layer. The third was a size 1.5 on a northeast aspect at 1800m failing down 40cm also on the early January layer. Natural activity is generally not expected on Sunday but could be possible on steep south facing slopes if the sun comes out in full strength in the afternoon. Newly formed storm slabs and a recently reactive persistent slab are both expected to be sensitive to human-triggering on Sunday.

Snowpack Summary

Recent snowfall and strong winds created storm slabs in many places and wind slabs on features lee to the southerly winds. This new snow has also added load and stress to the already volatile persistent slab. A layer of surface hoar from mid-January is expected to underlie recently formed storm slabs in many areas. The recently destructive layers of surface hoar from early-January are now typically down 70-120cm and remain highly reactive. These layers have the potential for wide propagations and remote triggering, and smaller avalanches have the potential to easily step-down to one of these layers. The mid and lower snowpack are generally strong and well settled below these layers. Snowpack depths are variable across the region and shallow snowpack areas may have weak facetted crystals near the ground.

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.