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Avalanche Forecast

Archived

Mar 26th, 2016–Mar 27th, 2016

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

Regions

Little Yoho.

http://www.pc.gc.ca/apps/scond/Cond_E.asp?oID=23022&oPark=100092#il

The Little Yoho region has an overall deeper and more settled snowpack than the main range just to the East.  Watch for thin areas where a larger avalanche can be triggered.  See the Special Public Avalanche Warning link above for more details.

Weather Forecast

Not much change Sunday with freezing levels to 1900m and light SW winds.  A NE flow will move in Sunday night into Monday which will drop 10-20cm East of the divide but will likely only result in 5-10cm for the Little Yoho region.

Snowpack Summary

A crust lies on solar aspects into the alpine and on shady aspects up to ~2000m where it disappears. In the top meter of the snowpack, several buried suncrusts exist and may still be a concern on west, south and east aspects but in general the snowpack is well settled. Low elevation snowpacks (Field ice climbs) are isothermal and slushy in the PM.

Avalanche Summary

No new avalanches reported in the Little Yoho region over the past 24-hours. Climbing in Guinness Gully Thursday revealed a lot of old, wet debris in the gullies on Mt. Dennis and this should be expected during the afternoon periods over the next few days. Loose wet avalanches to size 1.5 on steep solar aspects on Mt. Field Saturday PM.

Confidence

Forecast snowfall amounts are uncertain on Monday

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.

Cornices

Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.