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Avalanche Forecast

Archived

Feb 13th, 2017–Feb 14th, 2017

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

Regions

Little Yoho.

With temperatures climbing and the potential for sunny periods on Tuesday, expect both Wind Slabs and the deep Persistent Slabs to become more sensitive to natural and human triggering.

Weather Forecast

Warming temperatures are likely to be the dominant input over the next few days. Expect freezing levels to approach Treeline on Tuesday with diminishing cloud cover however West winds should also be increasing and may moderate the temperatures . Watch local conditions carefully and consider heating both at your level and on the slopes above you.

Snowpack Summary

40-60 cm of new snow over the past 11 days followed by extreme SW winds has created new snow slabs over various layers of weaker facets, surface hoar, and buried wind layers. In below treeline areas, this new snow load is sitting on a snowpack entirely made up of facets and depth hoar.

Avalanche Summary

Numerous natural and explosive triggered avalanches were observed and reported throughout the forecast region up to size 3 in the last 72hrs. Avalanche control Saturday found thin, sensitive hard slabs and touchy cornices in the alpine. Soft slabs over the persistent weak layers failed easily at treeline and easily entrained loose snow BTL.

Confidence

Freezing levels are uncertain on Wednesday

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.

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.