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Avalanche Forecast

Archived

Jan 12th, 2024–Jan 13th, 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.

Check out our Forecasters' Blog about factoring extreme cold into your trip plans. Small problems can spiral out of control quickly in these conditions.

Confidence

Moderate

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

Around 15 cm of new snow fell in the region early in the week. It added to an existing skiff of snow atop a widespread crust that exists up to 1400 m. South and west-facing alpine slopes are generally scoured but may see some wind transporting snow onto them with the northerly winds. The snowpack is generally shallow with multiple crusts. Pockets of deeper, wind-loaded 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

Friday night

Cloudy with no new snow, southwesterly 5-15 km/h, treeline temperature low of -33°C.

Saturday

Mostly sunny with no new snow, northeasterly winds 5-10 km/h, treeline temperature high of -24°C.

Sunday

A mix of sun and cloud, with no new snow, northeasterly winds 5-10 km/h, treeline temperature high of -23°C.

Monday

Cloudy, with no new snow, southwesterly winds 20-30 km/h, treeline temperature high of -12°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.