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Avalanche Forecast

Archived

Jan 30th, 2020–Jan 31st, 2020

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

Regions

North Columbia.

Avalanche danger is expected to become HIGH before the end of the day as heavy precipitation, strong winds, and rising temperatures make their way into the region. Be aware of conditions changing over the day, especially in overhead terrain.

Confidence

High -

Weather Forecast

Thursday night: Cloudy with flurries bringing 10-15 cm of new snow. Moderate to strong southwest winds. 

Friday: Cloudy with increasing snowfall bringing 25-30 cm of new snow, transitioning to rain below about 1700 metres, continuing overnight. Strong southwest winds. Alpine high temperatures approaching 0 as freezing levels climb to 1800-2000 metres.

Saturday: Cloudy with continuing flurries bringing 15-25 cm of new snow and new snow totals to 40-60 cm, closer to 5-10 cm below 1500 metres. Moderate to strong southwest winds shifting northwest and easing. Alpine temperatures dropping to about -7 as freezing levels fall from 1900 to 1000 metres over the day.

Sunday: Cloudy with isolated flurries and a trace of new snow. Light southwest winds. Alpine high temperatures around -10.

Avalanche Summary

Due to continuous stormy weather, there have been daily avalanches reported in the region. Most of these have been storm and wind slab avalanches, on all aspects, at all elevations. They have been triggered by humans, explosives, and naturally.

There was a notable avalanche reported in the northern Monashees on Saturday. It was a natural size 4 persistent slab avalanche. It was triggered by a wind slab avalanche that stepped down to a deeper layer.

There was also a notable size 3 persistent slab avalanche in the northern Selkirks on Saturday that was triggered by explosives on a southwest aspect in the alpine.

Looking forward, heavy precipitation, strong winds, and rising temperatures will promote increasing natural avalanche activity on Friday. During this time, occasional persistent slab releases such as those mentioned above may result from avalanche activity in surface snow layers.

Snowpack Summary

35-45 cm of new snow is expected to fall at higher elevations in the region by end of day on Friday. The new snow will cover wind affected recent snow at alpine and upper treeline elevations while rain saturates the surface below about 1700 metres.

The mid and lower snowpack is generally well settled and strong, however, there is a weak layer of surface hoar currently buried 90 to 170 cm deep. This layer is suspected to have produced a few sporadic large avalanches recently reported in the north of the region.

Terrain and Travel

  • Storm slab size and sensitivity to triggering will likely increase through the day.
  • Avoid exposure to overhead avalanche terrain during periods of heavy loading from new snow, wind or rain.
  • Be alert to conditions that change with elevation.

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.

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.