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Avalanche Forecast

Archived

Dec 26th, 2019–Dec 27th, 2019

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

Regions

North Columbia.

Watch for fresh wind slabs in upper elevation terrain. Natural persistent slab activity has slowed way down, but large avalanches may still be sensitive to human triggering. If you are increasing your exposure to avalanche terrain, do it gradually as you gather information.

Confidence

Moderate - Uncertainty is due to the fact that persistent slabs are particularly difficult to forecast.

Weather Forecast

It’s mostly dribs and drabs of snow for the next few days with increased wind in the higher alpine terrain features. A bigger storm is on the horizon as we enter the New Year.

THURSDAY NIGHT: Freezing level at valley bottom, moderate to strong south/southwest wind in the alpine, potential for 4 to 12 cm by Friday morning.

FRIDAY: Overcast, freezing level at valley bottom, light variable wind at most elevations, moderate to strong northwest wind in high elevation alpine terrain, 1 to 5 cm of snow possible during the day.

SATURDAY: Broken cloud cover, freezing level at valley bottom, light variable wind at most elevations, moderate to strong west/northwest wind in high elevation alpine terrain, no significant precipitation expected.

SUNDAY: Scattered cloud cover, freezing level at valley bottom, light variable wind, no significant precipitation expected.

Avalanche Summary

On Wednesday control work produced some size 2.5 persistent slab avalanches on both north and south facing features between 2100 and 2400 m, crowns were up to 120 cm in depth. Natural avalanches size 2.5 to 3 were also observed in the neighboring Glacier National Park in steep terrain, these avalanches were running to the top or middle of runnouts.

Avalanche activity has really tapered off, but avalanches during and just after the storm were spectacularly large and destructive. On Tuesday some natural avalanches up to size 2 were observed in ridge top start zones on a northwest facing slope around 2100 m. There were also some rather spooky size 2 storm slabs on east/southeast facing slopes down in the trees at 1900 m. On Monday natural avalanche activity from size 2 to 3 was observed on a variety of aspects above 2100 m. Control work produced avalanches from size 2 to 4 that involved all elevation bands, some mature timber was taken out by very large avalanches.

Snowpack Summary

The North Columbias received upwards of 80 cm from last weekend's big storm which is slowly settling into a slab. There is now a great deal of uncertainty as to how quickly the snowpack is regaining strength. Anywhere from 100 to 160 cm of snow is now resting on a widespread layer of large, feathery, surface hoar which we're calling the "December 11th Surface Hoar." Activity on this interface has really tapered off, but this layer produced some very large natural avalanches during and just after the storm. 

A combination of surface hoar, crust & facets formed in late November is now over 170 cm deep. This layer is likely trending toward dormancy.

Terrain and Travel

  • Start on smaller terrain features and gather information before committing to bigger terrain.
  • Avoid convexities, steep unsupported terrain and rocky outcroppings.
  • Fresh wind slabs will likely form throughout the day, diligently watch for changing conditions.
  • Avalanche hazard may have improved, but be mindful that deep instabilities are still present.

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.