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Avalanche Forecast

Archived

Jan 8th, 2014–Jan 9th, 2014

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

Regions

South Rockies.

Confidence

Fair - Intensity of incoming weather systems is uncertain on Saturday

Weather Forecast

Tonight and Thursday: Light precipitation for tonight, a trace during the day tomorrow and it should pick up Thursday night with the arrival of another system . Around 5-10 mm. in water equivalent is forecasted for that period. Light to moderate W and SW winds are forecasted. Freezing levels should remain at the surface.Friday: Light precipitation becoming moderate later, most of it should fall late Friday night and the next day. Moderate W winds for the day. Freezing levels are forecasted to rise close to 1000 m during the day.Saturday: The zonal flow keeps feeding systems to the province. However, this system looks stronger and could leave bigger amounts of precipitation than the previous ones. Temperature are expected to be warmer at first and winds to be strong.

Avalanche Summary

No new avalanches were reported yesterday. A detailed incident report about the Corbin area near miss on Jan. 5th is available here.

Snowpack Summary

The light snow amounts forecasted before the weekend and moderate winds from the W-SW will most likely create new windslabs below ridgetop in the alpine and cover older windslabs from previous wind event. Surface sluffing could also be possible within the new snow in sheltered areas. The facet/crust layer down 80-100 cm at treeline and below treeline and the depth hoar layer in the alpine seems ripe for skier or sledder triggering on E aspects. Multiple recent natural and human triggered avalanches on this aspect is a good sign of this instability. When tested and observed, the surface hoar layer down 70 cm is showing signs of healing (grains are rounding and snowpack test are not as planar as they used to be). The South Rockies field team has posted a new blog with some good info and pictures about the recent avalanche incident and about current conditions. Click here to read it.

Problems

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.

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.