Avalanche Forecast

Issued: Jan 5th, 2020 4:00PM

The alpine rating is considerable, the treeline rating is considerable, and the below treeline rating is considerable. Known problems include Storm Slabs and Persistent Slabs.

Avalanche Canada ahanna, Avalanche Canada

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There is some uncertainty as to how the recent storm snow is bonding to the old surface and how buried weak layers have reacted under the new load. 

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Summary

Confidence

Low - Uncertainty is due to the limited number of field observations.

Weather Forecast

Sunday night: Flurries accumulating up to 5 cm, moderate west wind, alpine temperatures around -12 C.

Monday: Sunny with cloudy periods, light to moderate west to northwest wind, alpine high temperatures around -12 C.

Tuesday: Mix of sun and cloud with isolated flurries, light variable wind, alpine high temperatures around -10 C.

Wednesday: Mix of sun and cloud with isolated flurries, light to moderate variable wind, alpine high temperatures around -10 C.

Avalanche Summary

A widespread avalanche cycle up to size 3 was reported from the Howson range during the storm on Friday with avalanches up to size 2 observed below treeline. This cycle is likely to have occurred throughout the southern part of the region on Friday and Saturday, where more than 40 cm of snow fell on Friday. 

Before the storm, reports of persistent slab avalanches associated with buried surface hoar were trickling in, from Ashman, Telkwa and Howson areas. They included natural and artificially triggered avalanches ranging in size from 1.5-3, and have occurred on all aspects mainly at treeline but also in the alpine. The new snow load will increase the size and consequences of avalanches on these layers.

Snowpack Summary

40-60 cm of recent storm snow has been highly wind affected in the alpine. Expect to find deep wind loaded pockets below ridgetops and the lee sides of exposed features. 

A couple of layers of surface hoar are now buried 50-100 cm below the surface in sheltered areas around treeline. Reports of avalanche activity on these layers before the last storm suggest they may be active, especially now that they are under additional snow load.

Terrain and Travel

  • Closely monitor how the new snow is bonding to the old surface.
  • Be careful with wind loaded pockets, especially near ridge crests and roll-overs.
  • Be aware of the potential for large avalanches due to the presence of buried surface hoar.
  • Uncertainty is best managed through conservative terrain choices at this time.

Problems

Storm Slabs

An icon showing Storm Slabs

40-60 cm of recent storm snow and strong winds have likely formed deep pockets of storm slab in lee features in the alpine and treeline. Watch for solar triggering of recent snow on solar aspects during periods of sun. Even after natural storm cycle avalanche activity starts to taper off, storm slab avalanches will remain sensitive to human triggering.

Aspects: All aspects.

Elevations: All elevations.

Likelihood

Possible - Likely

Expected Size

1 - 2.5

Persistent Slabs

An icon showing Persistent Slabs

A couple layers of surface hoar are now buried 50-100 cm deep, with uncertainty around their distribution outside of the treeline elevation band. There is uncertainty as to how the buried weak layers have reacted to the new load of storm snow. Human triggering of weak layers at this depth is definitely possible and would result in large, high consequence avalanches.

Aspects: All aspects.

Elevations: Treeline.

Likelihood

Possible

Expected Size

2 - 3

Valid until: Jan 6th, 2020 5:00PM

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