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Avalanche Forecast

Archived

Mar 30th, 2017–Mar 31st, 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 and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
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.

Regions

Northwest Coastal.

The next pulse of snow, rain at lower elevations, and wind is forecast overnight. Expect avalanche danger to increase as the storm slabs deepen.

Confidence

Moderate - Forecast snowfall amounts are uncertain on Friday

Weather Forecast

Overnight: Cloud developing this evening combined with strong southwest winds and 5-10 cm of new snow by morning. Friday: Overcast with 15-20 cm of new snow above 1000 metres combined with strong southwest winds. Saturday: 15-20 cm of new snow with freezing levels dropping below 1000 metres and winds backing off to moderate southwest. Sunday: Another 5-8 cm of new snow with moderate westerly winds.

Avalanche Summary

Numerous natural storm slabs up to size 2.0 were reported on Wednesday, as well as one natural cornice size 2.0 in the south of the region, and one natural cornice size 3.0 near Stewart. Two natural persistent slab avalanches were reported northwest of Terrace on Tuesday that released down 100 cm and failed in shallow rocky areas adjacent o large slopes.. On Sunday, a machine-triggered Size 3 (with crown approximately 2m thick) was reported in the South Douglas area just north of Terrace on a northwest aspect near 1400m. The slab is suspected to have run on the late February interface and involves an incredible story of survival. Click here for details.

Snowpack Summary

Storm slabs continue to develop in the alpine and at treeline. Warm daytime temperatures have created moist snow at treeline and wet snow below treeline. The February 21st persistent weak layer continues to be a concern for triggering large avalanches. This combination of crust and weak facets is now down 100-150 cm, and may be triggered by light additional loads in shallow weak spots adjacent to large terrain features. The snow below treeline may become weak and release as loose wet avalanches or wet slabs in steep unsupported terrain features.

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.