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Avalanche Forecast

Archived

Apr 11th, 2023–Apr 12th, 2023

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

Regions

North Columbia, South Columbia, Blue River, Clearwater, Clemina, Esplanade, Jordan, North Monashee, North Selkirk, Shuswap, West Purcell, Badshot-Battle, Central Selkirk, Goat, Gold, Kokanee, North Okanagan, Retallack, Valhalla, Whatshan.

It's the time of year when avalanche conditions vary widely by elevation. Increase caution as you reach your target of upper elevations where melt freeze crust is thinner or absent. This is also where recent storm snow may still react to human triggers.

Confidence

High

Avalanche Summary

Reports from Monday included a few more storm slab avalanches that were noted for being triggered remotely (from a distance). These ranged from 20-50 cm deep but seem to have shared the same storm interface failure plane, which has been noted as surface hoar and as facets in some of the more prominent reports of touchy conditions from the past few days.

At least one new persistent slab was observed with a 100 cm crown fracture in the western Purcells. Further observations may reveal more activity at this deeper layer in the days to come.

Saturday and Sunday saw an overall increase in wind slab and storm slab activity as the storm touched down in the region. This MIN gives a good sense of the conditions initially at play.

Looking forward, elevations that saw moderate to heavy rain should see avalanche activity drastically reduce with overnight cooling periods. Areas where new surface crust is very thin and especially where it is absent may still harbour upper snowpack instabilities.

Snowpack Summary

Continuing convective flurries will bring light new snow amounts to the region through Tuesday night, adding to about 30-50 cm of recent storm snow. Recent high freezing levels much of this fell as moist heavy snow or rain below about 2000 m, leading to a new melt freeze crust here and below. Expect wind slabs to have formed from southwest winds higher up where snow was light enough to be transported.

On southerly aspects at treeline, there is another widespread crust now buried 30 to 50 cm deep. On north-facing slopes at treeline and above this layer may exist instead as faceted snow or surface hoar in sheltered areas. A second surface hoar layer found closer to 60 cm deep has been reactive to human triggering primarily in the Selkirks on northeasterly slopes from 1700 m to 2100 m. Wednesday was the last day that there was notable activity on this layer but this may have changed during the storm.

The mid-snowpack is generally strong but the lower snowpack is a different story. The November facets are still prominent at the base of the snowpack. This layer remains a concern in rocky, shallow, or thin to thick snowpack areas at treeline and above.

Weather Summary

Tuesday night

Cloudy with continuing flurries bringing a trace to 10 cm of new snow. Light southwest winds.

Wednesday

Mainly cloudy with scattered flurries bringing a trace of new snow. Light west winds shifting northwest. Treeline high temperatures around -3 with freezing levels to 1400-1600 m.

Thursday

Mainly sunny. Light west or southwest winds. Treeline high temperatures around -1 with freezing levels to 1400-1600 m.

Friday

Cloudy with isolated flurries bringing a trace to 5 cm of new snow. Light southwest winds. Treeline high temperatures around 0 with freezing levels to around 1700 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Approach steep open slopes at and below treeline cautiously, buried surface hoar may exist.
  • In areas where deep persistent slabs may exist, avoid shallow or variable depth snowpacks and unsupported terrain features.
  • When a thick, melt-freeze surface crust is present, avalanche activity is unlikely.

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.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.