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Avalanche Forecast

Archived

Apr 1st, 2023–Apr 2nd, 2023

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

Regions

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

Give the storm snow another day to settle before venturing into larger or more committing terrain. Saturday's storm dropped variable amounts of snow across the region, and spotty spring squalls will continue for a few days, so observe your local conditions and let that inform your terrain choices.

Confidence

Moderate

Avalanche Summary

On Saturday, northeast of Clearwater, several small (size 1) rider triggered storm slab avalanches were reported on steep rolls.

East of Revelstoke, explosives avalanche control produced a few small to large avalanches (size 1.5-2) in steep, north facing alpine terrain.

In neighboring Glacier National Park, several large (size 2-2.5), loose avalanches were reported in steep alpine chutes. They started in drier snow, and entrained wet snow as they ran below treeline.

On Thursday, north of Revelstoke, a large (size 2), naturally triggered, deep persistent slab avalanche was reported. It occurred on a steep, north facing slope in the alpine, below a large cliff face, and it is possible that it was triggered by a cornice fall.

Snowpack Summary

10-25 cm of recent snow sits over a thin crust on steep slopes facing the sun right up into the alpine. Moderate southwest wind may have formed deeper deposits of snow on leeward slopes. On high, north-facing terrain, wind slabs may sit over facets and surface hoar.

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

Following Saturday's storm, a generally convective weather pattern will mean that the next few days will have spotty areas of cloud and light snowfall, or quick bursts of intense snowfall, but it also might be sunny, and everything could change at the drop of a hat.

Saturday Night

Cloudy, spotty clear areas. Trace of snow expected. Moderate localized flurries bringing up to 5 cm in isolated locations. Light southwest ridgetop wind, possibly moderate at high elevations. Freezing level at valley bottom, treeline low around -9°C.

Sunday

Mostly cloudy, possibly clear in the southeast corner of the forecast area. Trace of snow expected. Moderate localized flurries bringing up to 5 cm in isolated locations. Very light variable ridgetop wind. Freezing level rising to around 1300m. Treeline high around -5°C.

Monday

Mostly cloudy. Possible trace of snow expected. Up to 5cm in isolated areas. Light northwest ridgetop wind. Freezing level at valley bottom overnight, rising to around 1300m.

Tuesday

Mostly Sunny. Possible trace of snow expected. Up to 5cm in isolated areas. Light north or northwest ridgetop wind. Freezing level at valley bottom overnight, rising to around 1500m.

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.
  • Keep in mind the crust offers an excellent bed surface for avalanches.
  • In areas where deep persistent slabs may exist, avoid shallow or variable depth snowpacks and unsupported terrain features.

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.