Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Jan 10th, 2020–Jan 11th, 2020

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

Regions

Northwest Inland.

Seek out sheltered low density snow while it lasts, strong winds are in the forecast. Keep eyes open for signs of instability like shooting cracks or recent avalanches telling you the new snow has settled into a reactive slab.

Confidence

Moderate - Uncertainty is due to the limited number of field observations.

Weather Forecast

Friday night: Cloudy with isolated flurries bringing a final trace of new snow. Light winds shifting from southwest to northwest.

Saturday: Mainly cloudy with isolated flurries and a trace of new snow. Light northwest winds shifting northeast and increasing overnight. Alpine temperatures around dropping to -20 or lower by late afternoon.

Sunday: Sunny. Moderate northeast winds, becoming strong at ridgetop. Alpine temperatures around -28.

Monday: Sunny. Moderate east winds. Alpine temperatures around -30.

Avalanche Summary

Reports from the region are limited, however a widespread avalanche cycles are likely to have occurred over the past weekend and again on Friday as a result of rapid loading during each storm. Friday's activity is suspected to have been focused toward higher elevation, wind-exposed areas.

Before the last storm, reports of persistent slab avalanches associated with buried surface hoar were trickling in, from Ashman, Houston Telkwas, and the Howsons. They included natural and artificially triggered avalanches ranging in size from 1.5-3, and have occurred on all aspects, mainly at treeline. Loading from recent snowfall has increased the size and consequences of avalanches that may occur on these layers.

Looking forward, new snow from Friday's storm will remain our primary concern. Under forecast cool temperatures the new snow may continue to react to human triggers as dry loose sluffs. Greater danger should be expected in areas where winds have redistributed snow into deeper and more reactive slabs. 

Snowpack Summary

Up to 35 cm of new snow is expected to accumulate in the region by the end of the day on Friday. The new snow has mainly buried wind-affected surfaces at alpine and upper treeline elevations. It may cover a new layer of surface hoar at sheltered lower elevations or a thin sun crust on steeper south-facing slopes.

Below the new snow interface, 40-60 cm of older, wind-affected storm snow is expected to be forming a good bond with the interface below it.

A concerning pair of surface hoar layers are currently buried about 75-120 cm below the surface in sheltered areas around treeline. Reports of avalanche activity on these layers before the last storm suggest they may be active. The new load delivered by Friday's storm has increased this potential.

Terrain and Travel

  • Avoid freshly wind loaded terrain features.
  • Be aware of the potential for large avalanches due to the presence of buried surface hoar.

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.