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Avalanche Forecast

Archived

Apr 6th, 2016–Apr 7th, 2016

Alpine
Below Threshold.
Treeline
Below Threshold.
Below Treeline
Below Threshold.
Alpine
Below Threshold.
Treeline
Below Threshold.
Below Treeline
Below Threshold.
Alpine
Below Threshold.
Treeline
Below Threshold.
Below Treeline
Below Threshold.

Regions

Little Yoho.

Expect the hazard to rise towards HIGH as skies clear and temperatures rise on Thursday. There may be an opportunity for some corn skiing if timed right. Plan to finish early over the next few days.

Weather Forecast

Skies will clear through Thursday as another warm ridge of high pressure arrives and temperatures will skyrocket for Thursday afternoon and Friday. The hazard will again rise towards HIGH with heating and as crusts break down.

Snowpack Summary

A skiff of new snow on top of surface crusts that remained intact today except at valley bottom elevations. The morning snowpack is strong when frozen, but this can rapidly break down with warming. In many places the snowpack is sitting on a deep persistent layer of facets that has been avalanching with solar heating over the previous week.

Avalanche Summary

Another day of cool weather. Tuesday's trip through Surprise Pass showed a snowpack locked up from the cold temperatures. Sunshine reports isolated wind slabs in the immediate NW lees of ridgelines 20-50 cm thick. They were less reactive today, but may be more touchy in the warmer days to come. Similar conditions may exist on the Wapta.

Confidence

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.

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.

Cornices

Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.