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Avalanche Forecast

Archived

Apr 2nd, 2015–Apr 3rd, 2015

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

Regions

Sea To Sky.

Deep persistent weaknesses are still producing avalanches. Big alpine features cannot be trusted.

Confidence

Good

Weather Forecast

5-10 cm of snow is expected on Friday and another 5-10 cm by Saturday morning, before things start to dry out with a mix of sun and cloud on Sunday. Daytime high freezing levels are expected to hover around 1500 m for the forecast period. Moderate southwesterly alpine winds are expected on Friday then light but gusty southwesterlies for the weekend.

Avalanche Summary

Reports from Wednesday include explosive triggered storm slab avalanches up to Size 2, and one Size 3 persistent slab release on the mid-March persistent weakness.

Snowpack Summary

Up to 25 cm of low density storm snow is sitting on a thin breakable crust that caps 30-40 cm of recent moist snow on rain crust buried last Saturday. Reports suggest this 5 cm thick solid rain crust exists up to at least 2200m. Strong southwest winds have shifted these new accumulations into touchy wind slabs in exposed terrain. A facet/crust persistent weakness buried mid-March is down approximately 70-130 cm and is still producing hard but sudden results in snowpack tests. This remains the chief concern amongst avalanche professionals in the region due to it's potential for very large avalanches.

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.

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.