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Avalanche Forecast

Archived

Feb 17th, 2021–Feb 18th, 2021

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

Regions

Vancouver Island.

Numerous reports of size one avalanches mainly associated with wind slabs on NE to NW aspects at tree line elevations both naturally and human triggered. Widespread reports of settlements (whoomphing) at below treeline and treeline elevations on all aspects. One report of possible skier triggered avalanche size 1.5 from Sunday Feb 14 in the west bowl of Mt Cain on the feature called Sliders. No reports of injuries or lost gear at this time.

Past Weather

The past three days have seen the temperatures climb slowly back toward our normal cool/mild island winter levels. Light to moderate amounts of snow has fallen (10-20 cm in most zones). Winds have varied from NW to SE and have been light to strong.

Weather Forecast

Wednesday sees winds changing from the NW flow that has chilled us all, back to our regular SE flow that will blow in the next winter snow storm, with new snow falling Thursday through Friday. Wednesday - no new snow fall, winds strong NW falling to light SE, temps for 1500 m -4 to -7, freezing level 0 to 800 m.Thursday - 5 to 15 cm of new snow, winds moderate to strong SE, temps for 1500 m -6 to -1, freezing level 400 to 800 m.Friday - 5 to 20 cm of new snow, winds moderate to strong SSW, temps for 1500 m -4 to -5, freezing level 500 to 1000 m.

Terrain Advice

Avoid or be careful when entering wind loaded zones near ridge tops (especially open bowls and gullies) as wind slabs have and will continue to form over the next few days. Winds will come from multiple directions and load all aspects vs just the typical flow from the SE. Watch steep small bits of terrain associated with openings in the forest, as buried weak layers (surface hoar and facets) are now loaded with new snow and more is coming. Avoid exposure to terrain traps in these openings, as even small slides associated with them can magnify the potential for injury in these bits of small terrain.Multiple recent avalanche accidents in the states with many injuries and deaths have resulted from a well know touchy persistent buried weak layer. When interviewing survivors many mentioned their mental state and decision making processes (risk tolerance) were to some degree affected by Covid (either making them more numb to the warning signs due to their desire to get out, or a concern over not getting another chance to get out if restrictions to travel tighten). Be sure to do a good and thorough analysis of your decision making process, factor in weather and snowpack and don't forget the human factors.

Snowpack Summary

From Sat Feb 13 until Tuesday night Feb 16 approximately 20 to 30 cm of new cold light snow fell on a old crust surface. Winds both from the SE and the NW have moved this light snow to either form wind slabs or strip zones down to the crust. Cold temperatures have eaten away at the thickness and strength of the crust that capped the two persistent weak layers in our mid snowpack to varying degrees based on location, aspect and elevation. Higher temperatures warmed the snow surface in below treeline elevations Tuesday leaving a slight crust and also saw trees shed their snow loads making travel in the forest unenjoyable.

Snowpack Details

  • Surface: Variable surface conditions from wind slab to exposed crust up high. Some nice pow still lingers in pockets.
  • Upper: Low density cold snow from previous storms
  • Mid: A rotting variable thickness crust with weak snow crystals (2 facet layers and some surface hoar) below.
  • Lower: Well settled

Confidence

Moderate - Many reports submitted for the entire forecast zone, weather models in agreement but uncertainly lies around the future sensitivity of the persistent weak layers that lie in our snowpack.

Problems

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.

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.