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Avalanche Forecast

Archived

Mar 20th, 2020–Mar 21st, 2020

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

Regions

North Columbia.

Clouds may temper day-time warming. Minimize exposure to cornices and steep slopes that face the sun during the warmest part of the day.

Confidence

High - Confidence is due to a stable weather pattern with little change expected.

Weather Forecast

Friday night: Clear, light west wind, alpine temperature -13 C, freezing level valley bottom.

Saturday: Increasing cloud, light northwest wind gusting moderate at ridge-tops, alpine temperature -6 C, freezing level 1300 m.

Sunday: Increasing cloud, isolated flurries in the afternoon with trace accumulations, light southwest wind gusting moderate at ridge-tops, alpine temperature -6 C, freezing level 1300 m. 

Monday: Mostly cloudy, 5-10 cm of snow, light west wind, alpine temperature -7 C, freezing level 1300 m.

Avalanche Summary

Over the past several days, avalanche activity was reported as natural loose dry or loose wet avalanches size 1-2 running in steep, sun-exposed terrain in the alpine. One large (size 2) slab avalanche released naturally as a result of strong solar radiation on a south aspect at 2500 m. There were also several large cornice failures on northerly aspects (up to size 2.5).

If you decide to travel in the backcountry, consider sharing your observations via the Mountain Information Network (MIN) to supplement our data stream as operators are shutting down. Even just a photo of what the day looked like would be helpful.

Snowpack Summary

Surface conditions are highly variable with a mix of sun crusts, moist snow, hard wind slabs, and soft faceted snow. Reports indicate that surface hoar may be developing on the surface on sheltered, shady slopes. Cornices are large, looming, and weakening with warm temperatures and strong solar radiation.

A widespread weak layer of surface hoar buried in late February is now 60-100 cm deep. Sheltered north, northeast, and east facing slopes near treeline are the most likely locations to find this layer. Avalanche activity on this layer was last reported on March 8th. There is a low likelihood of triggering an avalanche on this layer, but the consequences of doing so would be high.

Terrain and Travel

  • Back off slopes as the surface becomes moist or wet with rising temperatures.
  • Pay attention to cornices and give them a wide berth when traveling on or below ridges.
  • Small avalanches can have serious consequences in extreme terrain. Carefully evaluate your line for wind slab hazard before you commit to it.
  • Make observations and assess conditions continually as you travel.

Problems

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.