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Avalanche Forecast

Archived

Feb 15th, 2024–Feb 16th, 2024

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

Regions

Sea To Sky, Brandywine, Garibaldi, Homathko, Spearhead, Tantalus.

Keep your guard up in steep open terrain! Wind slabs are bonding poorly to underlying layers.

Confidence

High

Avalanche Summary

There has been a steady stream of small (size 1 to 1.5) wind slab avalanches observed over the past few days. Natural avalanches were triggered by outflow winds, while human-triggered avalanches have occurred on a range of aspects. Most slabs were 20 to 30 cm thick, with some failing on a buried surface hoar layer.

Snowpack Summary

Sun and wind are creating variable surface conditions. Exposed terrain is being scoured by northeast wind and forming small wind slabs on south and west facing slopes.

Roughly 30 cm of snow sits above large surface hoar and/or faceted crystals at treeline and above. A widespread, supportive crust exists 30 to 40 cm below the surface.

The snowpack is strong and bonded below this crust.

Weather Summary

Thursday Night

Clear skies. 30 km/h east ridgetop wind. Treeline temperature -7 °C.

Friday

Sunny. 30 km/h southeast ridgetop wind. Treeline temperature -3 °C.

Saturday

Mostly cloudy. 30 km/h southeast ridgetop wind. Treeline temperature -2 °C with freezing level around 1200 m.

Sunday

Cloudy with 1 to 2 cm of snow. 15 km/h west ridgetop wind. Treeline temperature -2 °C with freezing level around 1200 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Be careful with wind slabs, especially in steep, unsupported and/or convex terrain features.
  • Back off if you encounter whumpfing, hollow sounds, or shooting cracks.
  • Keep your guard up at lower elevations. Wind slab formation has been extensive.

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.