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Avalanche Forecast

Archived

Feb 28th, 2023–Mar 1st, 2023

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 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.

Regions

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

Wind slabs in exposed areas, a dodgy interface just waiting for storm slabs to settle over it, power sluffing where slabs haven't formed, and a lurking deep persistent slab problem. It's a lot to think about! Seems like seeking out the soft, sheltered snow and managing its predictable sluffing might be the best strategy for Wednesday.

Confidence

High

Avalanche Summary

It's been a busy time for avalanche activity in the region with almost all operators reporting some variation of the theme of a natural and skier-triggered avalanche cycle as 40-70 cm of new snow this weekend settled into touchy storm slabs in some areas and produced powerful dry loose releases with rider traffic in areas where slabs hadn't quite formed. Improved travel conditions on Monday allowed for more observations of the aftermath of the cycle, generally observed to have produced avalanches to size 2.5 (large!) and for the most part confined to the depth of new snow. A few operators noted the cycle being less widespread than expected.

Clear skies last week allowed for observations of many deep persistent slab avalanches as well as explosive control missions, which produced large to very large (size 2 to 3.5) avalanches. Another one was triggered in Glacier National Park on Monday. These avalanches have been occurring on all aspects and generally between 2200 m and 2800 m in elevation. Although many of these avalanches have occurred in unrideable terrain, they are evidence that the weak basal snowpack is still triggerable. Riders should continue to avoid thin snowpack areas, which are often found near ridgelines.

Looking forward, storm slabs from the weekend may remain sensitive to human triggering a bit longer than usual, owing to the weak faceted snow they overlie. Otherwise we expect surface instabilities to gradually become more focused toward wind loaded areas.

Snowpack Summary

Stormy conditions over the weekend brought up to about 40-80 cm of new snow to the Monashees, closer to 20-50 cm in the Selkirks, along with strong southwest wind. The new snow buried an interface from the recent cold period which includes faceted (sugary) surface snow, small surface hoar in sheltered areas, and widespread heavy wind effect and wind slabs in exposed terrain from recent northeast winds. A significant number of operators in the region have been hesitant to drop storm slab problems from their assessments, likely owing to this problematic interface.

Around 100 to 130 cm of snow may now rest on a small layer of surface hoar crystals that was buried mid-February. This layer is most likely found around treeline elevations in areas sheltered from the wind. This layer generally appears to be dormant now but could still be capable of producing avalanches in isolated areas. 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. The likelihood of human triggering this layer is currently low given its depth. However, alarming reports like this one from Glacier National Park continue to trickle in, confirming it is still best to avoid steep, thin, rocky slopes near ridges at alpine and upper treeline elevations.

Weather Summary

Tuesday

Brief clearing before clouding over again. Light northwest winds shifting southwest and increasing.

Wednesday

Cloudy with isolated flurries, increasing in late afternoon and overnight. Light west winds shifting southwest and increasing. Treeline high temperatures around -9.

Thursday

Cloudy with continuing snowfall bringing 10-25 cm of new snow, including overnight amounts, greatest in the north of the region. Moderate southwest winds, potentially strong in the alpine. Treeline high temperatures around -7.

Friday

Cloudy with continuing flurries bringing 5-10 cm of new snow, including overnight amounts. Light to moderate southwest winds. Treeline high temperatures around -8.

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.
  • Watch for signs of slab formation throughout the day.
  • Be aware of the potential for loose avalanches in steep terrain where snow hasn't formed a slab.
  • Avoid shallow, rocky areas where the snowpack transitions from thick to thin.

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.

Loose Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.