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Avalanche Forecast

Archived

Jan 14th, 2024–Jan 15th, 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

East Kakwa, Tumbler.

In areas with enough snow to ride, thick to thin snow pack transitions remain a concern.

Confidence

Low

Avalanche Summary

No new or recent avalanches have been reported, however there are very few field observations coming from this forecast area.

If you go out in the backcountry, please consider sharing your observations on the Mountain Information Network (MIN).

Snowpack Summary

15 cm of snow fell in the region early last week which sits on a widespread crust that exists up to 1400 m. South and west-facing alpine slopes are generally scoured with only a bit of recent wind transported snow from this weekend's northerly wind.

The snowpack is generally shallow with multiple crusts. Pockets of deeper snow may be found near ridges, gully features, and established avalanche paths.

Average snowpack depths at treeline vary between 20 to 80 cm.

Weather Summary

Sunday Night

Clear, with no new snow, northwest alpine wind 20-50 km/h, treeline temperature high of -25 °C.

Monday

Mix of sun and cloud, with no new snow, west alpine wind 30-50 km/h, treeline temperature high of -18 °C.

Tuesday

Mostly cloudy with up to 7 cm of snow, east alpine wind 10-20 km/h, treeline temperature -15 °C.

Wednesday

Mix of sun and cloud with no new snow, northeast alpine wind 30-60 km/h, treeline temperature high of -25 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Expect shallow snow cover that barely covers ground roughness.
  • Avalanche danger is often elevated in alpine gullies where snow has accumulated.

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.