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Avalanche Forecast

Archived

Apr 11th, 2022–Apr 12th, 2022

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.

Wind slabs likely exist in steep terrain at higher elevations.

Confidence

Moderate - Forecast snowfall amounts are uncertain.

Weather Forecast

MONDAY NIGHT: Cloudy with snowfall, accumulation 2 to 5 cm, 10 km/h northeast wind, alpine temperature -10 C.

TUESDAY: Cloudy with snowfall, accumulation 5 to 10 cm with local amounts up to 20 cm possible, 20 to 40 km/h northeast wind, alpine temperature -11 C.

WEDNESDAY: Cloudy with snowfall, accumulation 5 to 10 cm, 10 to 20 km/h northeast wind, alpine temperature -9 C.

THURSDAY: Mix of sun and cloud with no precipitation, 10 km/h northeast wind, alpine temperature -10 C.

Avalanche Summary

On Sunday, avalanche activity was limited to cornices, releasing naturally or by explosives. Otherwise, evidence of old wet avalanches was observed.

Looking forward, riders could trigger wind slabs in steep terrain features at higher elevations. Best to stay well back of cornices too, as they are very large at this time of year.

Snowpack Summary

New snow on Tuesday will accumulate onto the 10 to 20 cm of dry, wind-affected snow that sits above a hard melt-freeze crust in alpine terrain. Wind slabs may be found in steep, lee terrain features from strong northeast to southeast wind. At and below treeline, snow will accumulate onto a hard melt-freeze crust.

A melt-freeze crust that formed late March to early April is found 60 to 100 cm deep. Avalanches were sliding on this layer last week, but activity has since decreased. The likelihood of triggering this layer is low given the cool weather.

There are no deeper concerns at this time.

Terrain and Travel

  • Carefully evaluate steep lines for wind slabs.
  • Pay attention to cornices and give them a wide berth when traveling on or below ridges.
  • When a thick, melt-freeze surface crust is present, avalanche activity is unlikely.

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.