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Avalanche Forecast

Archived

Mar 24th, 2013–Mar 25th, 2013

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

Regions

South Columbia.

Confidence

Good

Weather Forecast

Synopsis: Stable pattern under a ridge of high pressure expected to continue. In other words, little change.Overnight and Monday: Dry, light westerly winds, solid overnight freeze (-10 to -15 C) with daytime warming (around -5 in alpine). Monday freezing level rising to near 1300 m but above freezing temperatures likely to go higher on slopes facing the sun.Tuesday: essentially a nearly identical forecast to Monday except a couple of degrees warmer.Wednesday: some high cloud drifting in. Tuesday night may stay warmer limiting the overnight freeze and crust recovery at treeline elevations and lower.

Avalanche Summary

Loose wet solar triggered avalanches reported on southerly aspects. Failing cornices are common. Most didn't trigger additional slab avalanches although a few did, including a size 4 just north of the region (likely involving the March 10 surface hoar/crust interface).A fatal snowmobile triggered size 3 avalanche was reported in the southern Purcell mountains. No details are available at this time.

Snowpack Summary

Moist snow may be found on solar aspects up to about 2200 metres. New melt/freeze crusts are developing due to cold clear nights and strong solar radiation during the day. The recent storm amounts are between 40-80 cms at higher elevations. Strong winds overnight and early Wednesday morning developed thick pockets of wind slab at higher elevations. Cooling temperatures have promoted bonding to the moist snowpack at lower elevations. New cornice growth is reported to be extensive and weak. Expect natural cornice falls that may trigger weak layers that are buried down a metre or more on slopes below. The new storm load may trigger the March 10th weak surface hoar layer.

Problems

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.

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.