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Avalanche Forecast

Archived

Jan 8th, 2017–Jan 9th, 2017

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

Regions

Sea To Sky.

The incoming storm will form new wind slabs and increase the avalanche danger at higher elevations.

Confidence

Moderate - Intensity of incoming weather systems is uncertain on Monday

Weather Forecast

SUNDAY: Flurries starting in the evening, moderate southeast winds. Alpine temperatures around -4. MONDAY: 10 cm of new snow by the morning with another 10-15 possible during the day. Moderate to strong southwest winds. Alpine temperatures around -6. TUESDAY: Clearing in the morning, light northeast winds, alpine temperatures around -12 Celcius. WEDNESDAY: Sunny with light northerly winds. Alpine high temperatures near -12 Celcius.

Avalanche Summary

No new avalanches observed.

Snowpack Summary

5-15 cm of snow from Friday covers a variable surface with a mix of soft wind slabs, hard wind slabs, sastrugi, faceted snow, and even some surface hoar. Last week's winds reverse loaded many terrain features and formed stubborn wind slabs on a surprising range of aspects. An interface of faceted (sugary) snow and surface hoar was buried on Boxing Day and can be found up to 100 cm deep. Recent observations suggest the snow has bonded well to this interface. Snowpack layers below this interface are also generally well bonded.

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.