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Avalanche Forecast

Archived

Jan 27th, 2020–Jan 29th, 2020

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

North Rockies.

Monitor new snow depth and wind redistribution closely as Wednesday's storm makes its way into the region. Be prepared to dial back your terrain selection if snowfall exceeds forecast amounts. Avoiding wind-exposed areas will be a good strategy for the day.

Confidence

Moderate - Forecast snowfall amounts are uncertain.

Weather Forecast

Monday night: Clear periods. Light to moderate southwest winds, easing into the morning.

Tuesday: Becoming cloudy with scattered flurries bringing up to 5 cm of new snow, mainly in the south of the region. Light southwest winds. Alpine high temperatures around -7.

Wednesday: Cloudy with flurries bringing 5-10 cm of new snow, with possible locally enhanced amounts, continuing and easing overnight. Moderate to strong south or southwest winds. Alpine high temperatures around -5.

Thursday: Mainly cloudy with isolated flurries and a trace of new snow, increasing a bit overnight. Light to moderate south or southwest winds, increasing overnight. Alpine high temperatures around -5.

Avalanche Summary

Reports from the past several days have highlighted wind slab problems at higher elevations, with observations from Bullmoose, Hasler, Torpy, and Pine Pass all showing strong evidence of the problem. These reports suggest a good transition from more widespread storm slab conditions observed a day earlier in the Sentinel Pass area.

Explosives control work in the Sentinel Pass area on Friday revealed a touchy storm slab problem at alpine and treeline elevations. Seven out of eight explosives produced avalanches from size 2 to 2.5 (large). Crown fracture depths were approximately 40 cm, the height of recent snowfall in the area. None of these avalanches stepped down to a persistent weak layer.

Looking forward, our wind slab problem won't get much of a chance to stabilize before new snow and elevated winds complicate matters again on Wednesday. Forecast snowfall varies over the region, so it will be important to assess new snow depths over the day on Wednesday and again on Thursday morning to determine the scale of any new wind slab problem or whether the greater concern is a skiff of snow obscuring slabs lingering from the last storm.

Snowpack Summary

Recent snow has settled with warm temperatures and been blown around by wind from various directions, resulting in wind slabs on all aspects at and above treeline. These are expected to be on a positive stabilizing trend under the current pattern of mild weather, but new snow and wind should shake things up on Wednesday.

A weak layer of surface hoar buried in late December remains a concern but seems to be gaining strength. This layer has been found across much of the North Rockies region, but has seemed to be more problematic in particular areas, such as around McBride and the McGregors/Torpy. It seems to be most readily found in sheltered treeline features 50 to 150 cm below the surface.

Terrain and Travel

  • Be careful as you transition into wind affected terrain.
  • Seek out wind sheltered terrain below treeline where you can avoid wind slabs and find great riding.
  • Avoid steep slopes when air temperatures are warm, or solar radiation is strong.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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.