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Avalanche Forecast

Archived

Jan 6th, 2021–Jan 7th, 2021

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

Regions

Little Yoho.

Clear, dry weather pattern over the next few days will help settle the recently created windslabs. A few spotty persistent weak layers exist in the snowpack and should be considered when choosing your objective

Weather Forecast

A ridge is building over the next 3 days. Expect benign weather: light westerly alpine winds, clear skies and cool overnight lows in the -15 to -20 range.

Snowpack Summary

5-10 cm on Wed brings recent storm snow totals to 20-50 cm at treeline. This sits on a spotty stellar/surface hoar layer in some sheltered locations. Wind effect in open areas at treeline and in the alpine. Two weak layers from early Dec persist 50-100 cm down. These have been generally unreactive but still giving hard sudden planar results

Avalanche Summary

Poor visibility today meant limited observations in the alpine, but strong to extreme winds and 5-10 cm snow likely meant avalanches were running. Test pits at treeline show moderate resistant planar results down 30-45 on a preserved stellar/ surface hoar interface and moderate to hard sudden planar results down 50-70 cm on surface hoar/ facets.

Confidence

Wind effect is extremely variable

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.

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.