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Avalanche Forecast

Archived

Apr 15th, 2016–Apr 16th, 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.

Watch for a weak freeze Saturday night to prime conditions for poor travel and likely an avalanche cycle Sunday and Monday as a ridge brings warm air and sunny skies.

Weather Forecast

Friday evening should see a reasonable freeze with a continued light, slightly unstable, westerly flow. Freezing levels will reach 2500m Saturday afternoon. Expect a weak freeze with warm air invading. Sunday watch for SIGNIFICANT HEATING: calm winds and clear skies allowing strong solar effect combined with freezing levels in excess of 3500m.

Snowpack Summary

We are into a spring cycle for most of the Little Yoho area except in high north facing alpine. Occasional pockets of deep instability may still be encountered and triggered from shallow locations during warm periods of the day. 5cm of recent snow overlies crusts that extend to all but North aspects aboveĀ  about 2600m.

Avalanche Summary

No new avalanches observed or reported today.

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.

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.