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Avalanche Forecast

Archived

Jan 8th, 2014–Jan 9th, 2014

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

Regions

Glacier.

Weather Forecast

A series of disturbances will start making their way east over our region. Flurries will bring 5-10cm today/tonight. Light alpine winds. Freezing levels hovering between 1000-1200m.

Snowpack Summary

Surface hoar that formed over the last few days has now been buried by 2-3cm of snow overnight. Settlement of recent storm snow continues in upper snowpack. Thin sun crust was observed on steep south aspects. Mid pack is well settled. Lower snowpack still has more facetted crystals but is showing signs of strength more typical for this region.

Avalanche Summary

A couple of size 2-2.5 slabs from high elevation, steep start zones on Mt Tupper were observed yesterday. Riders reported surface sluffing from steeper terrain.

Confidence

Due to the number and quality of field observations

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.