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Avalanche Forecast

Archived

Mar 26th, 2017–Mar 27th, 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 possible, human triggered probable.

Regions

Northwest Coastal.

With the new snow load, persistent slab problems continue to rear their ugly head. Conservative terrain use is essential & stay aware of overhead hazards.

Confidence

Moderate - Timing, track, or intensity of incoming weather system is uncertain

Weather Forecast

We're looking at a series of systems impacting the region throughout the forecast period. The winter storm train keeps rolling into town! MONDAY: Snow in the afternoon (10cm). Strong south wind, freezing level around 1100 m with alpine temperature around -3 C. TUESDAY: 15-25 cm Monday overnight into Tuesday afternoon, strong southwest wind, freezing levels 1200m. WEDNESDAY: Lingering flurries (5-10 cm possible) moderate south wind, freezing levels 1100m, alpine temperature around -4 C.

Avalanche Summary

On Sunday, a machine-triggered Size 3 (with crown averaging 1.5m thick) was reported north of Terrace on a northwest aspect near 1400m. The slab is suspected to have run on the late February interface.On Saturday, several wind slabs to Size 1.5 were reported on (east) northeast aspects in the north of the region. On Friday, a spooky Size 3.5 persistent slab with impressive propagation was remote-triggered north of Terrace at 1500m elevation. See here for more details in this excellent post.A significant concern remains the potential for persistent slab avalanches triggered by people. See the forecaster blog for advice on managing a low probability - high consequence problem (here) and the accompanying photos (here).In addition to the daunting persistent slab problem, the incoming weather pattern is looking to continually build fresh storm slabs.

Snowpack Summary

Fresh storm slabs (up to 40cm thick) developed at treeline and above, while cornices grew larger during another March storm: Weekend totals brought 10-20cm of new snow and moderate southwest / southeast winds. This recent snow sits on a crust on solar aspects and below 1000 m.Snow may still be poorly bonded to a 40 cm deep crust and surface hoar interface from mid-March, however, the late-February interface has been the more troublesome persistent layer. It's composed of facets, crust, and surface hoar roughly 70-140 cm deep and is still reactive throughout the region, especially in shallower areas around Stewart and Bear Pass. See the Avalanche Summary above for a good example of this persistent problem re-awakening.

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.