Posted:
Jan 1, 2020 @ 6:52 am

 An avalanche warning has been issued for the southern Mission, southern Swan, Rattlesnake, and southern and central Bitterroot mountains.The avalanche danger for the west central Montana backcountry is High. Human triggered avalanches are certain. The avalanche hazard is increasing with continued snowfall. Travel in avalanche terrain is not recommended. Avalanches may run long distances and avoid runout zones.

Happy New Year, this is Jeff Carty with an avalanche warning for January 01, 2020.This avalanche warning is valid for 24 hours. The avalanche warning will either be extended or terminated at 0600 on January 02, 2020. This danger rating does not apply to operating ski areas, expires at midnight tonight, and is the sole responsibility of the U.S. Forest Service.

Weather and Snowpack

The snow is here. What started lightly on Tuesday has intensified and is bringing considerable snowfall to the mountains creating dangerous avalanche conditions. 

Up to 2.3″ of snow water equivalent (SWE) fell as up to 12″ of heavy snow last night, adding considerable stress to a weak snowpack.  1-3″ more SWE is expected by Thursday night, more than doubling the extra weight that has already been added to the snowpack. Strong westerly winds with extreme gusts are accompanying it, rapidly increasing the load on leeward slopes. Temperatures will increase Wednesday with rain possible above 6000 feet drastically increasing thaw instabilities.

Clear skies and cold temps Sunday night created extensive surface hoar on all aspects in the forecast area. Compounding this is a crust under the new snow that sits on near-surface facets. What this means is that there are multiple low strength, low friction sliding surfaces that the new snow is landing on. 

The snowpack varies widely throughout the forecast area, from very shallow in the southern Bitterroot to near seasonal norms in the Swan. Depths are widely varied from bowl to bowl and aspect to aspect. Monday in the Rattlesnake, the size of the depth hoar on north aspects, under a 51-inch snowpack, was alarming, while some south aspects between 6000-7000 feet had as little a 1 foot of snow. All of it, regardless of depth, contains a combination of facets and crusts. 

Despite the poor structure, we have not seen widespread avalanches, mainly due to a lack of slab and weight on top of it. As new snow accumulates, adding weight, the likelihood of avalanches rapidly increases. The incoming snow will consolidate into a slab quickly due to its density. 

Storm slabs that slide on the surface hoar/new snow/crust/facet combo may step down to weak layers deep in the snowpack and trigger much larger slides. 

High winds are creating slabs many feet thick in leeward and cross-loaded areas.

The weak structure of the underlying snowpack can not be trusted. Avoid all slopes over 30º and be very aware of overhead hazard. The surface hoar that the new snow is landing on can propagate long distances, and it may be possible to trigger avalanches from flat ground, above or below a slope. If deeper instabilities fail they may create very large slides. Early season conditions increase the likelihood of trauma if caught in a slide.

Our primary concern is storm slab avalanches. A very close second is persistent slab avalanches. Both may happen simultaneously.

Please, share any avalanche or condition observations on our public observations page.

Ski and ride safe.

 

 

 

 

READ FULL ADVISORY  

Problem 1 -

  • TYPE

    storm-slabs

    Storm Slabs

    Release of a soft cohesive layer (a slab) of new snow which breaks within the storm snow or on the old snow surface. Storm-slab problems typically last between a few hours and few days. 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.

  • SIZE

    4-5

    2 (Large)

    The potential size of avalanche resulting from this problem.

  • LIKELIHOOD

    Likelihood-6

    Likely/Very Likely

    The likelihood of an avalanche resulting from this problem.

  • ADDED DANGER

    Increased Slope Danger

    Increased/Added Danger

    There is an increased risk of avalanches on these slopes:

    N - North
    NE - Northeast
    E - East
    SE - Southeast
    S - South
    SW - Southwest
    W - West
    NW - Northwest

A very weak combo of facets, crust, and surface hoar underlie the new snow. Storm slab avalanches are certain. Heavy snowfall accompanied by wind and warm temperatures is rapidly overloading weak layers.

Over the past few days, multiple small loose snow and point release avalanches have been observed. These are traveling fast on the crust/facet layer and indicate how low the friction is. 

It’s slippery. 

Storm snow that consolidates is likely to release as a slab on this layer and may propagate long distances. 

Storm slab avalanches may trigger larger persistent slab avalanches.

As new snow depths increase, so does the risk. Keep an eye on snow accumulation, pay attention to the density, and stick to slopes under 30º. Travel in avalanche terrain is not recommended.

Don’t let fresh snow tempt you out on steep slopes prematurely.

Problem 2 -

  • TYPE

    persistent-slabs

    Persistent Slabs

    Release of a cohesive layer of soft to hard 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 Persistent, Deep-Slab.

  • SIZE

    6-7

    3 (Large-Very Large)

    The potential size of avalanche resulting from this problem.

  • LIKELIHOOD

    Likelihood-4

    Possible/Likely

    The likelihood of an avalanche resulting from this problem.

  • ADDED DANGER

    Increased Slope Danger

    Increased/Added Danger

    There is an increased risk of avalanches on these slopes:

    N - North
    NE - Northeast
    E - East
    SE - Southeast
    S - South
    SW - Southwest
    W - West
    NW - Northwest

Facets continue to develop in the lower snowpack. In shaded colder slopes, these have become large, well-developed depth hoar. 

Many crusts also exist in the snowpack, providing both bed surfaces and areas that promote the growth of facets.  

Stability tests continue to show:

  • Low to moderate strength
  • Low friction (high energy)
  • High propagation likelihood
  • Poor structure

This problem is unpredictable, will be with us for a while, and is increasing in destructive potential as it gets buried further.

The new snow is rapidly loading weak layers, and the likelihood of larger slides is increasing. 

Don’t let the new snow tempt you out on steep slopes prematurely, the likelihood of surviving a slide that releases on one of the persistent weak layers is diminishing quickly.

Avalanches in the new snow layer could step down and trigger slides in the persistent weak layers.

VIDEO

FORECAST & OUTLOOK

Increased precipitation throughout Wednesday

1-3″ of snow water equivalent possible by Thursday.

Temps:

4000′-6000′, 32º to 41º

6000′-8000′, 27º to 35º

Rain possible to above 6000′

Temps cooling tonight and Thursday

This information is the sole responsibility of the Forest Service and does not apply to operating ski areas. The avalanche danger rating expires at midnight tonight but the information can help you make a more informed decision regarding travel in avalanche terrain for the next few days.

Our advisory area includes National Forest System lands in the Bitterroot Mountains from Lost Trail Pass north to Granite Pass, the Rattlesnake Mountains north of Missoula and the Southern Swan and Mission Mountains near Seeley Lake, MT. Avalanche information for the Lookout Pass/St. Regis Basin area is available from the Idaho Panhandle Avalanche Center.