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Avalanche Forecast

Archived

Mar 13th, 2020–Mar 14th, 2020

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

Regions

Northwest Coastal.

Strong outflow winds have formed wind slabs on atypical aspects. Buried weak layers warrant a cautious mindset and terrain use strategy.

Confidence

Moderate - Uncertainty is due to how the snowpack will react to the forecast weather.

Weather Forecast

Friday night: Clear, strong outflow winds from the northeast, alpine temperature near -22 C.

Saturday: Clear, strong outflow winds from the northeast, alpine high temperature near -12 C, freezing level near 500 m.

Sunday: Clear, light northeast winds, alpine high temperature near -6 C, freezing level rising to 2500 m overnight.

Monday: Clear, light northeast winds, alpine high temperature -1 C, freezing level near 2500 m.

Avalanche Summary

With continuing strong outflow winds, wind slabs are expected to remain to possible to human trigger. 

In the aftermath of the storm earlier in the week, avalanches releasing on surface hoar layers have continued. Operators reported several large (size 2-3) avalanches breaking on both the March 9th and March 1st surface hoar layers from human and explosive triggers. Several of these avalanches were remotely-triggered. Check out this MIN from the Shames area for a helpful example.

During intense periods of solar radiation on Thursday, small (size 1-1.5) loose wet avalanches ran on steep, sun-exposed slopes. Cold air may limit solar influence on Saturday, but use caution if the snow moistens. 

Two very large (size 2.5-3) natural glide slab avalanches were observed along the Terrace highway on Friday. Maintain conservative margins to avoid areas with glide cracks.

Snowpack Summary

Strong arctic outflow winds are building fresh wind slabs in a reverse-loading pattern. Last week's storm delivered 30-60 cm of new snow to the region with strong southwest winds creating ample snow available for wind transport. 

The recent snow is sitting on a weak layer of surface hoar buried 30-60 cm deep in many areas, especially in sheltered areas at treeline and below treeline. See this MIN from the Shames area that shows this layer when it was on the surface. Observers have reported widespread whumpfing and propagation in snowpack tests on this March 9th surface hoar, confirming its propensity for human triggers. 

There are several additional layers of surface hoar that are now buried 70-120 cm and 110-160 cm deep that may also be the most prominent around treeline. On south through west facing slopes, this surface hoar may be sitting on a crust, which may increase the potential for triggering avalanches on these layers. Below about 1000m, the recent new snow is sitting on a melt-freeze crust.

A weak layer of facets that formed in January may be found about 150 to 200 cm deep, and an early season melt-freeze crust lingers at the base of the snowpack. These layers have produced a few very large natural and explosive triggered avalanches over the past two weeks.

Terrain and Travel

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Be aware of the potential for large avalanches due to the presence of buried surface hoar.
  • Use extra caution around cornices: they are large, fragile, and can trigger slabs on slopes below.

Problems

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.

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.