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Avalanche Forecast

Archived

Jan 19th, 2013–Jan 20th, 2013

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

Regions

Little Yoho.

Ski quality has gone downhill due to the winds and warm temperatures. Ice climbers avoid pockets of hard windslabs on steep features in the alpine. SH

Weather Forecast

Light to mod. NW winds Sunday (Front ranges may have E winds Sunday AM) . A trace of snow is possible over the front ranges, but overall dry conditions are in the forecast .  Alpine temps around -10C Sunday with freezing levels near valley bottom.

Snowpack Summary

10-20+ cm variable windslabs from strong W/NW winds over last 3 days. 25-35cm over Jan 6 interface of facets and/or surface hoar (preserved W of divide treeline and below). Helen Ridge profile at treeline found mod. compression results on a 15cm surface windslab, with no results below on a mainly facetted snowpack. Thin sun crust on steep S slopes.

Avalanche Summary

No new avalanches reported today.  Winward slopes have been scoured to the bare rocks in many areas East of the divide.

Confidence

on Sunday

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.