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Avalanche Forecast

Archived

Feb 23rd, 2013–Feb 24th, 2013

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

Regions

Little Yoho.

There's variability in danger in the region. Areas immediately along the Divide saw up to 20cm of new snow, locally increasing the danger rating. East of the Divide saw a dusting, thus, a lower danger. If it dumped where you are, keep your eyes open.

Weather Forecast

Tomorrow we should see increasing clouds with possibly 5-10cm late in the day. Moderate west winds will accompany this storm. Monday will have unsettled convective cells rolling through, with little in the way of snow for us.

Snowpack Summary

Up to 20cm reported over last 24 hours in the alpine immediately along the Divide. Some thin ridgetop soft wind slab formation in immediate ridge top lees. This snow sits on top of wind slabs, both soft and hard, in alpine areas. Thin snowpack areas at all elevations are very weak and faceted, as are most below treeline areas up to 1900 meters.

Avalanche Summary

Large sloughing was observed off the Stanley Headwall, likely due to strong winds at ridge-top. Experienced climbers in the area said they were large enough to knock climbers off their intended routes. Point releases from steep terrain were observed further south in Kootenay, all in the recent snow.

Confidence

Forecast snowfall amounts are uncertain

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.

Loose Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.

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.