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Avalanche Forecast

Archived

Mar 4th, 2023–Mar 5th, 2023

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

Regions

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

Choose conservative terrain this weekend as storm snow continues to show reactivity.

Avoid wind loaded features, and watch for strong sunshine affecting south facing slopes - reactivity will increase if skies clear.

Check out the latest Forecaster Blog for the latest on the Deep Persistent Slab Problem.

Confidence

Moderate

Avalanche Summary

Avalanche activity has continued throughout the week, as storm snow kept stacking up. Activity included storm slabs, wind slabs in wind loaded features and loose dry avalanches from steep sheltered terrain.

Natural and human triggered avalanches continue to be reported, mostly to size 2. Most avalanche activity is isolated to the storm snow or old/new interface, while several larger natural slab avalanches were reported to size 3.5 likely failing on the buried facets and surface hoar layers.

Deep persistent slab avalanche reports continue to trickle in over the week, to size 3. This evidence indicates the low probability but very high consequence weak basal snowpack is still active. Avalanches have occurred on all aspects and generally between 2200 m and 2800 m in elevation. Reports commonly noted the variation in depth - indicating that areas where the snowpack is shallow and rocky, or where it varies from thick to thin rapidly are still to be avoided. A fatal size 3 avalanche occurred near Invermere on Wednesday, which is directly adjacent to this forecast region.

Snowpack Summary

Storm snow from this week has been redistributed by recent southwest winds into deeper deposits on north and east facing aspects. Current easterly winds are expected to build deposits on west facing slopes as well, resulting in variable wind loading patterns. This storm snow sits over wind effected surfaces, a thin sun crust on steep south facing slopes.

Around 50-90 cm deep a layer of small surface hoar exists in lower elevation sheltered areas. Elsewhere heavily wind effected surfaces exist, with faceted (sugary) snow from the late February Arctic blast.

Another small layer of surface hoar is buried 70-130 cm deep from mid February. This layer is most likely found around treeline elevations in areas sheltered from the wind. These two layers have shown reactivity, producing avalanches and concerning test results. The remainder of the mid-snowpack is generally strong.

A layer of large and weak facets that formed in November is deeply buried. Found near the base of the snowpack it is very slow to gain strength. The likelihood of human triggering this layer is currently low given its depth. However deep persistent slab avalanches continue to occurr, confirming it is still best to avoid steep, thin and rocky slopes at alpine and upper treeline elevations.

Weather Summary

Saturday Night

Light southeast winds, gusting moderate. Freezing levels below valley bottom.

Sunday

Mostly sunny, especially in the north, with cloudy periods elsewhere. Moderate southeast winds ease over the day Freezing levels below 500 m, alpine high of -8 °C.

Monday

A mix of sun and cloud. Light southerly winds. Freezing levels around 800 m in the south, alpine high of -5 °C. Light snowfall possible in the afternoon.

Tuesday

Mostly cloudy with moderate southwest winds. Freezing levels rise to 1000 m. Alpine high temperature of -3 °C. Flurries in most areas.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Continue to make conservative terrain choices while the storm snow settles and stabilizes.
  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Minimize exposure to sun-exposed slopes when the solar radiation is strong.
  • Avoid shallow, rocky areas where the snowpack transitions from thick to thin.

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.

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.

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.