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Avalanche Forecast

Archived

Apr 10th, 2024–Apr 11th, 2024

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

Regions

Banff Yoho Kootenay, Little Yoho, Banff, East Side 93N, Kootenay, Lake Louise, LLSA, Sunshine, West Side 93N, Field.

Recent snow has been wind effected but soft snow can still be found on high north aspects. Watch for windslabs in immediate lees and heads up for solar warming if the sun is out!

Confidence

High

Avalanche Summary

Ski patrol at Lake Louise reported triggering windslabs in alpine lee features that were 10-30 cm deep up to size 1.5. Sunshine reported some small cornice failures with daytime warming.

The Feb 3rd persistent weak layer is a deeper layer that we have been monitoring. There have been three avalanches involving this layer in the last 10 days: a natural near Bow Summit, a skier remote in Purple Bowl and a skier accidental at the Cathedral Glades.

Snowpack Summary

Surface crusts exist on all solar aspects and up to ~2000 m on shaded north aspects. Above ~ 2000m on north aspects, 10-30 cm of dry, wind effected snow exists with windslabs on lee ridgetop features.

The midpack is generally well settled until the February 3 persistent weak layer which remains a concern for human triggering in shallow snowpack areas on northerly alpine aspects. In these areas, no crusts are found in the upper snowpack and the midpack remains thin and weak.

Weather Summary

Thursday - expect increasing cloud with flurries in the afternoon/evening and only trace amounts. Freezing levels (FL) will be between 2000-2200 m with moderate SW ridgetop winds.

Friday - scattered flurries continue with light to moderate SW wind. FL range 2100-2400 m.

Saturday - expect bands of high cloud and moderate west wind.

Click here for more weather info.

Terrain and Travel Advice

  • Remember that in the spring strong solar radiation and warm temperatures can weaken the snow in a matter of minutes.
  • Watch for wind-loaded pockets especially around ridgecrest and in extreme terrain.
  • Avoid thin areas like rock outcroppings where you're most likely to trigger avalanches failing on deep weak layers.

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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.