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Avalanche Forecast

Archived

Apr 24th, 2024–Apr 25th, 2024

Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

South Coast Inland, Brandywine, Garibaldi, Spearhead, Birkenhead, Duffey, South Chilcotin, Stein, Taseko.

Continuously assess conditions as you gain elevation. Winter conditions persist at higher elevations.

New wind slabs could form throughout the day where precipitation falls as snow.

Confidence

Moderate

Avalanche Summary

On Tuesday a natural cornice fall resulted in a size two avalanche on a northwest aspect.

If you have any recent photos or observations, please submit them to the Mountain Information Network, observations are limited in the spring.

Snowpack Summary

Up to 15 cm of new snow may accumulate on all aspects at higher elevations. The largest deposits will be found on north and east aspects in the alpine. This new snow may not bond well to the underlying crust. Below treeline rain will keep the snow surface wet or moist where snow still exists. Most below treeline terrain is already snow free.

Weather Summary

Wednesday Night

Mostly cloudy with trace to 2 cm of new snow at treeline and above. 10 to 30 km/h southwest alpine wind. Freezing level falling to 1300 m.

Thursday

Cloudy with up to 5 cm of new snow at treeline and above. 10 to 20 km/h south alpine wind.  Freezing level rising to 1800 m.

Friday

Cloudy with up to 5 cm of new snow in high alpine terrain. 5 to 15 km/h variable alpine wind. Freezing level rising to 2100 m.

Saturday

Cloudy with 5 cm of new snow at treeline and above. 25 to 50 km/h south alpine wind. Freezing level rising to 1800 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Be carefull around freshly wind loaded features.
  • When a thick, melt-freeze surface crust is present, avalanche activity is unlikely.
  • Expect shallow snow cover that barely covers ground roughness.
  • Minimize your exposure time below cornices.
  • The more the snow feels like a slurpy, the more likely loose wet avalanches will become.

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.