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Avalanche Forecast

Archived

Mar 9th, 2014–Mar 10th, 2014

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

Regions

South Coast.

Strong solar radiation and rising temperatures could trigger natural avalanche activity on south facing slopes during the day.

Confidence

Fair

Weather Forecast

Monday: Cloudy with possible flurries early followed by sunny breaks. The freezing level is around 1400 m. Winds are light from the W-NW. Tuesday: A mix of sun and cloud. The freezing level climbs from 1000 m in the morning to 1700 m in the afternoon. Winds are light and variable. Wednesday: A mix of sun and cloud. Temperatures should climb even higher with the freezing level as high as 2500 m. Winds are light from the SW.

Avalanche Summary

Several skier controlled slab avalanches up to size 2 were reported on Saturday. Most of these were within the recent storm snow and many propagated quite widely. There was also a report of a very large natural slab avalanche from a north aspect near the Coquihalla. This avalanche may have occurred during the last storm on Thursday. Heavy snow and strong winds on Saturday night probably kicked off another fairly widespread avalanche cycle.

Snowpack Summary

Coquihalla and south: Recent mild temperatures have resulted in rain to ridge top in many areas. It's likely that the upper snowpack below 1700-1800 m is saturated and/or contains several melt-freeze crusts. The early March melt-freeze crust is down 60-100 cm depending on elevation. There are no new snowpack tests on this layer to report; however, continued loading and mild temps should help stabilize this previous weak layer. Duffey Lake and north: Around 25-35 cm of new snow fell on Saturday night, with strong southerly winds and freezing levels jumping between 1400 and 1700 m. It's The early March melt-freeze crust is down 60-80 cm on north aspects up to 1800 m and south aspects up to 2200 m. The mid Feb weak layer is generally now found down 90-130 cm. Recent snowpack tests continue to give popping shears where this layer is less than 100 cm deep. Deeply buried weak layers of facets and depth hoar remain a concern on high alpine slopes with thin or variable snow cover.

Problems

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.

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.