THIS AVALANCHE FORECAST EXPIRED ON January 18, 2021 @ 11:07 pm
Avalanche Forecast published on January 18, 2021 @ 6:07 am
Issued by Mark Dundas - Flathead National Forest

Triggering a slide in yesterday's storm snow remains our main concern. Avalanches have the potential to run long distances on top of a crust. In areas without a stout near-surface crust, you can impact a buried weak layer 1-3' below the surface, resulting in a larger slide. On steep slopes, steer around areas harboring dense snow that doesn't bond to the underlying crust. When in doubt, default to lower angle terrain free of rollovers. 

2. Moderate

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Above 6500 ft.
Heightened avalanche conditions on specific terrain features. Evaluate snow and terrain carefully; identify features of concern.

2. Moderate

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5000-6500 ft.
Heightened avalanche conditions on specific terrain features. Evaluate snow and terrain carefully; identify features of concern.

1. Low

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3500-5000 ft.
Generally safe avalanche conditions. Watch for unstable snow on isolated terrain features.
    Heightened avalanche conditions on specific terrain features. Evaluate snow and terrain carefully; identify features of concern.
  • 1. Low
  • 2. Moderate
  • 3. Considerable
  • 4. High
  • 5. Extreme
Avalanche Problem 1: Storm Slab
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The Swan Range was walloped with a short duration high-intensity snowfall event Sunday morning. Observers noted a widespread thin storm slab avalanche cycle that ran on top of the 1/13 rain crust. The natural activity has ended, but riders can still trigger slides in Sunday's fresh snow. This should be a relatively easy problem to assess. Utilize hand pits and small test slopes to gauge the bonding between the new snow and the crust. On steep slopes, be alert for snow that feels dense and cracks under you. Slabs will be thickest in the usual wind-loaded spots - downwind of ridgelines, saddles, and cross-loaded features. Where the new snow is loose and unconsolidated, sluffs can run on very steep slopes. Staying off slopes directly above a terrain trap where these small slides can pile up deep debris is a good habit to develop.

Avalanche Problem 2: Persistent Slab
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We have not received a report of a slide failing on a buried weak layer since the 1/13 storm, but observations have been sparse. There are 2 layers of buried surface hoar we are monitoring. The most reactive one is approximately 1 foot below the surface with another 2-3 feet down. Unfortunately, the only way to know their existence is by digging into the snow. They generally appear as a thin grey stripe and fail during snowpit tests. In areas where the surface consists of a thick hard crust, it is unlikely that you or your machine's weight can impact them. Slopes without a crust, or where the crust is thin and breakable, are most suspect. If you are unsure, utilize terrain to your advantage by avoiding steep rollovers or slopes which end in a terrain trap. Stick to planar slopes less than 35 degrees in steepness for a safer experience.

Forecast discussion

A quick-hitting disturbance passed through our area yesterday morning. Precipitation and snow totals were modest, except for the Swan Range, which picked up 1.1” of water and 8” of snow in a 7-hour window at Noisy Basin. 

Let us take a closer look at these numbers. The density of the freshly fallen snow at Noisy Basin was approximately 14% (Density=mass/volume or 1.1/8  x 100). To help put this into context, Steamboat, Colorado boasts about its 6% champagne powder. The temperature at Noisy during the snowfall event was 27 - 28 F, which coincides with snow a bit on the heavy side. It is unusual for a storm slab to form in 6% snow, but more common in 14% snow. Denser snow = more cohesive snow. Now let’s look at the precipitation intensity. 8” of snow over a 7 hour period equates to over an inch of snow an hour. That is dumping! More, please! That rate exceeds the rule of thumb of a loading threshold of 1” per hour. The higher the precipitation intensity the greater the chance of failure (and fracture) in the fresh snow. 

An observer in the Swan noted a natural storm slab cycle with 4-6” crowns on top of the 1/13 crust. This cycle occurred because the more cohesive 14% snow was deposited at a high intensity leading to failure. Having a stout, slick rain crust for a sliding surface was the final ingredient required for a slab avalanche to occur. Perhaps there was a thin layer of weak snow on top of the crust which added fuel to the fire. Off to the storm slab races, went the Swan.

Blase was in the southern Whitefish Range with FAC interns Jeremy and Zach. They found dust on a stout crust on southerlies, up to 6” on a less robust crust on northerlies, and triggered sluffs skiing both of these aspects. They noted a widespread storm slab avalanche cycle from the Pineapple Express. Slides were generally D1 to D2 with 2 D3 slides in this heavily used backcountry location. 

In honor of Martin Luther King Jr. Day, I will leave you with a couple of his quotes that are appropriate for these times.

“The time is always right to do what is right.”

“The ultimate measure of a man is not where he stands in moments of comfort and convenience, but where he stands at times of challenge and controversy.

 

Weather and CURRENT CONDITIONS
weather summary

Expect a quiet day with seasonable temperatures, light winds, and partly cloudy conditions. A weak system may move into our area Tuesday night into Wednesday.

Two-Day Mountain Weather Forecast Produced in partnership with the Missoula NWS
For 5000 ft. to 7000 ft.
Monday Monday Night Tuesday
Cloud Cover: Partly Cloudy Mostly Clear Partly Cloudy
Temperatures: 20 to 26 deg. F. 10 to 13 deg. F. 18 to 24 deg. F.
Wind Direction: Northwest Northwest Southwest
Wind Speed: 11G22 9 14G30
Snowfall: 0" in. 0" in. 0" in.
Snow Line: 1500' 1000' 500'
Disclaimer

This forecast applies only to backcountry areas outside established ski area boundaries. The forecast describes general avalanche conditions and local variations always occur. This forecast expires at midnight on the posted day unless otherwise noted. The information in this forecast is provided by the USDA Forest Service who is solely responsible for its content.