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Avalanche Forecast

Archived

Apr 8th, 2024–Apr 9th, 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, human triggered possible.
Below Treeline
Below Threshold.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Below Threshold.

Regions

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

Some new snow and incoming wind will build fresh wind slabs on Tuesday. Following this, clear weather on Wednesday will activate said storm snow due to solar radiation and daytime warming.

Confidence

High

Avalanche Summary

Sunshine patrol reported ski cutting some small size 1 wind slabs in immediate alpine lee areas. Otherwise, no new avalanches were observed or reported on Monday.

It has been a week since the last skier triggered avalanches on the Feb 3rd persistent weak layer occured. These involved a skier remote in Purple Bowl and a skier accidental at the Cathedral Glades.

Snowpack Summary

New surface crusts on all solar aspects and up to 2500 m on north aspects are buried by a skiff of snow. On high north aspects 15-20 cm of recent storm snow remains dry with some wind effect near ridgecrests.

The February 3 persistent weak layer remains a concern for human triggering in shallow snowpack areas on northerly alpine aspects where no crusts are found in the upper snowpack and the midpack remains thin and weak.

Weather Summary

5-10cm of snow is expected on Tuesday. It will be accompanied by cool-ish temperatures of close to 0 in the valley and -10 at the ridge level. There is a good chance the wind will blow strong from the West, but at minimum, it will be moderate.

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.