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Avalanche Forecast

Archived

Mar 29th, 2015–Mar 30th, 2015

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

South Coast.

Variable precipitation amounts expected. If your riding area sees more than 20 cm new snow or 20 mm rain, consider the avalanche danger to be high. See this blog post for more info about the tricky persistent slab problem: http://bit.ly/1HHQrK2

Confidence

Fair - Intensity of incoming weather systems is uncertain

Weather Forecast

Only relatively light amounts of precipitation are expected to spill into the inland region from storms impacting the coast through this period. Monday: 1-3 mm expected in most areas during the day, maybe 5 mm on the Coquihalla, then an additional 5-10 mm overnight from 4pm Monday to 4am Tuesday. Freezing level around 1900 m, ridgetop winds around 60 km/h from the SW. Tuesday: Unstable air bringing convective showers is expected to bring highly variable precipitation. Seeing 10 mm from an intense shower is possible, as is getting no precip at all. Freezing levels are expected to drop to around 1200 m and winds are expected to diminish to around 35 km/h from the west. Wednesday: Mostly dry with the occasional light shower. Freezing levels around 1400 m, winds light northwesterly.

Avalanche Summary

On Saturday, two size 2 wind slab avalanches were reported from the north of the region. For a little over a week, there have been consistent reports of avalanches to size 2.5 occurring on the mid-March persistent weak layer. Some avalanches have occurred naturally and many have been remote triggered from up to 100m away.

Snowpack Summary

This region has a very serious persistent slab problem that exists under the upper layers of dense storm snow. Depending on how much recent snow has fallen, a facet/crust persistent weak layer buried mid-March lies anywhere from 40-120 cm below the surface. Avalanches have continued to run on this layer at upper treeline and alpine elevations, especially in the north of the region. Snowpack layers deeper than this critical interface are reported to be generally well-settled and strong.

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.

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.