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Avalanche Forecast

Archived

Mar 29th, 2017–Mar 30th, 2017

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

Regions

Northwest Coastal.

Recent storm slabs may become reactive if the warm March sun pops out during the day. Storm slabs may "step-down" and release persistent weak layers, resulting in large avalanches.

Confidence

Moderate - Timing or intensity of solar radiation is uncertain on Thursday

Weather Forecast

Overnight: Some light precipitation expected to continue overnight, with light northwest winds and freezing down to 500 metres by morning. Thursday: A weak ridge of high pressure should bring broken skies or scattered cloud along with light northwest winds and daytime freezing up to 1100 metres. Friday: The next storm moves onto the north coast bringing 5-10 cm of new snow by morning and another 10-15 during the day combined with strong southwest winds and freezing levels up to 1300 metres. Saturday: Continued stormy weather with 15-20 cm of new snow and strong southwest winds.

Avalanche Summary

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 avlanches or wet slabs in steep unsupported terrain features. Spring conditions may change quickly, especially if the sun pops out during the day and warms the slab above the weak layer.

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.