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Avalanche Forecast

Archived

Dec 25th, 2022–Dec 26th, 2022

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 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

Northwest Coastal, Kitimat, Nass, Rupert, Seven Sisters, Shames, Stewart, Howson, Microwave-Sinclair, Telkwa.

Another warm storm system starting Sunday night is expected to create dangerous avalanche conditions for Monday. The recent storm snow sits over a widespread weak layer which is expected to be increasing the reactivity and size potential of the new storm slabs.

Confidence

Moderate

Avalanche Summary

This MIN report from Saturday includes reports of numerous small storm slab avalanches but also shows an avalanche stepping down to an older weak layer.

On Saturday in the south of the region, numerous natural storm slabs up to size 2 were reported. In the north, a natural size 1.5 storm slab was reported and a size 1.5 storm slab was remotely triggered from 7 m away which was 30 cm thick. Around Bear Pass, a few natural wind slabs up to size 2 were observed. An assortment of natural loose dry activity was also reported.

This MIN report from Friday shows a small wind slab avalanche with a relatively wide propagation given the thin slab and suggests a poor bond between the new snow and the old surface.

Snowpack Summary

The new storm snow has buried a highly variable snow surface that had formed during the recent period of extended cold temperatures and outflow winds. This newly buried weak layer consists of widespread facets, patchy surface hoar in sheltered terrain, and heavily wind-affected surfaces in exposed terrain including wind-scoured and wind-pressed surfaces, old hard wind slabs, and sastrugi.

A layer of large surface hoar crystals, buried in early December, was found down 20 to 50 cm prior to the storm. This layer has previously produced small but remotely-triggered avalanches.

The lower snowpack is well consolidated below a crust that had formed in mid-November which can be found below around 1200 m elevation.

Both the early-December surface hoar and mid-November crust have been dormant recently but could wake up with the new load from the storm snow, and avalanches have the potential to step down to these deeper layers.

Weather Summary

A series of storm systems continues to impact the region with another wave of precipitation expected to arrive late Monday morning.

Sunday night

Precipitation 8-16 mm tapering off overnight, strong S-SW wind, freezing level around 1500 m with a potential inversion.

Monday

Precipitation 10-20 mm with potentially higher amounts for the SW of the region, strong SE-S wind, freezing level around 1500 falling to around 1000 m in the afternoon.

Tuesday

Mainly cloudy with a chance of isolated sunny breaks, moderate NE wind, freezing levels generally falling to around 500 m or lower.

Wednesday

Cloudy with light flurries, moderate SW wind, treeline high around -3 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Continue to make conservative terrain choices while the storm snow settles and stabilizes.
  • Storm snow and wind is forming touchy slabs. Use caution in lee areas in the alpine and treeline.
  • Storm slabs in motion may step down to deeper layers resulting in large avalanches.
  • The more the snow feels like a slurpy, the more likely loose wet avalanches will become.

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.

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.