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Avalanche Forecast

Archived

Mar 31st, 2024–Apr 1st, 2024

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

Regions

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

There is uncertainty about how powerful localized solar impact and daytime heating will be tomorrow. It is the time of year to start early and finish early, to optimize the coolest temperatures of the day.

Confidence

Moderate

Avalanche Summary

Some small loose dry/wet avalanches were observed in Yoho, otherwise, no avalanches were reported on Sunday.

Snowpack Summary

Up to 35 cm of snow over old sun crusts on solar aspects, with new solar crusts forming. On polar aspects, this snow sits over a layer of stellars/spotty surface hoar crystals and is worth monitoring.

Our main concern is shallow snowpack areas on northerly alpine aspects where the midpack is thinner/weaker, and triggering Feb 3 facet/crust layer and basal facets/depth hoar remains possible.

Deeper snowpack areas have few concerns.

Weather Summary

The sky will be mainly sunny thanks to the influence of an upper ridge. Freezing levels rise to above the treeline along most of the range during the day, lowering to the valley bottom at night. Moderate westerly ridgetop winds

Click here for more weather info.

Problems

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.

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.