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Avalanche Forecast

Archived

Feb 29th, 2024–Mar 1st, 2024

Alpine
Natural and human triggered avalanches likely.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.

Regions

Cariboos, North Rockies, Blue River, Clearwater, McBride, Premier, Quesnel, Sugarbowl, Clemina, North Monashee, McGregor, Renshaw, Robson.

Dangerous avalanche conditions persist at all elevations. The snowpack will remain primed for rider triggering as natural avalanches taper off.

Confidence

Moderate

Avalanche Summary

Numerous natural and rider-triggered storm slab and persistent slab avalanches size 1 to 3 have been reported the past few days in the alpine and treeline elevation bands on all aspects. Most of these occurred on the weak layer of faceted grains 60-100 cm deep sitting on a crust formed in early February. Several were reported as remotely triggered (from a distance).

As natural avalanche activity tapers, the snowpack will remain primed for rider-triggered avalanches.

Snowpack Summary

70 to 110 cm of recent snow sits on a variety of layers that it may not bond well to, including surface hoar in wind-sheltered terrain, weak facets, or a hard melt-freeze crust on sun-exposed south and west-facing slopes. A plethora of recent avalanche observations indicate the fresh snow is not bonding well to these layers. The wind has likely formed thicker deposits in lee terrain features near ridges.

A thick and hard widespread crust that formed in early February is buried 50 to 100 cm deep and is found up to around 2400 m. This crust may have a layer of facets above it, which makes it a troublesome avalanche layer.

The remainder of the snowpack is settled.

Weather Summary

Thursday Night

Cloudy with flurries, 5 to 15 cm of snow. 15 to 30 km/h southwest ridgetop wind. Treeline temperature -16 °C. Freezing level at valley bottom.

Friday

Mostly cloudy with sunny breaks and isolated flurries, 5 cm of snow. 15 to 25 km/h southwest ridgetop wind. Treeline temperature -9 °C.

Saturday

A mix of sun and cloud and isolated flurries. 15 to 25 km/h southeast ridgetop wind. Treeline temperature -8 °C.

Sunday

A mix of sun and cloud. 5 to 15 km/h southeast ridgetop wind. Treeline temperature -8 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Shooting cracks, whumphs and recent avalanches are strong indicators of an unstable snowpack.
  • Fresh snow rests on a problematic persistent slab, don't let good riding lure you into complacency.
  • Storm slabs in motion may step down to deeper layers resulting in large avalanches.
  • Use conservative route selection. Choose simple, low-angle, well-supported terrain with no overhead hazard.

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.

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.