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Avalanche Forecast

Archived

Apr 3rd, 2023–Apr 4th, 2023

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
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, Badshot-Battle, Central Selkirk, Goat, Gold, Kokanee, North Okanagan, Retallack, Valhalla, Whatshan.

The danger ratings below represent areas that see cloudy skies, and little to no new snow on Tuesday. Dynamic spring weather could bring you intense sun or snowfall, either of which would increase the avalanche danger.

Observe your local conditions and let that inform your terrain choices.

Confidence

Moderate

Avalanche Summary

No notable avalanches were reported before 4pm on Monday.

On Sunday, around the forecast area, the new snow was reported to be reactive to rider traffic. Numerous small to large (size 1-2), rider triggered avalanches were reported, all in the alpine, and mostly on northeast aspects.

Several reports mentioned that the storm snow was touchy, propagated easily, and had the potential for remote and sympathetic avalanches.

This Mountain Information Network (MIN) post describes a skier triggered avalanche near the far south end of the forecast area.

Snowpack Summary

Recent convective weather has resulted in variable snowfall amounts across the forecast area.

15-40 cm of mostly soft snow is settling over a widespread, thin crust except north facing slopes at treeline and above, where it sits on old, faceted surfaces, and surface hoar in some areas.

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

A generally convective weather pattern will mean that on Tuesday we'll see 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. Most notably, the eastern edge of the South Selkirks (East of Nakusp and Slocan), have the highest potential for sustained convective snowfall Monday night/Tuesday, and could see up to 20 cm of new snow.

Monday Night

Mix of clear and cloud. Possible trace of snow expected. Light variable ridgetop wind. Freezing level falling to valley bottom. Treeline low around -8°C.

Tuesday

Mostly cloudy. Possible trace of snow expected. Up to 20cm in isolated areas, see note above. Light variable ridgetop wind. Freezing level rising to around 1400m. Treeline high around -5°C.

Wednesday

Mix of sun and cloud. No new snow expected. Light west or southwest ridgetop wind, trending to moderate at higher elevations. Freezing level at valley bottom overnight, rising to around 1500m.

Thursday

Mostly cloudy. 0-2 cm of snow expected. Light to moderate southeast ridgetop wind, trending to strong southwest at higher elevations. Freezing level at valley bottom overnight, rising to around 1600m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Even a small avalanche can be harmful if it pushes you into an obstacle or a terrain trap.
  • Pay attention to isolated alpine features as well as cross-loaded features at treeline.
  • Make observations and assess conditions continually as you travel.
  • 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.