Posted:
Jan 14, 2021 @ 6:55 am

The avalanche danger in the west central Montana backcountry is high in wind loaded terrain above 7000′ and considerable in all other terrain. 

Good Morning. This is Jeff Carty with the West Central Montana Avalanche Center advisory on Thursday, January 14th, 2021. This advisory is sponsored by LB Snow. This advisory 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

Mountain temperatures range from 15º to 23º F this morning. Winds are moderate out of the west. The advisory area has received no new snow overnight except for Twin lakes in the central Bitterroot that received o.6″ of snow water equivalent (SWE).

It’s been an eventful 48 hours. Stuart SNOTEL in the Rattlesnake reported a total of 2.2″ SWE, a massive load for the weakest snowpack in the forecast area. Winds reached 125mph on Mt. Sentinel, the Swans saw winds of 65mph and gusts to 101mph and, Lolo Pass had winds to 106mph. Temperatures reached 39ºF at 6400′ at Twin lakes and 34ºF at 7400′ on Stuart. Rain reached at least 7400′ in elevation. Above 7600′ in the central Bitterroot, there was up to 14″ of new snow. Skiing and riding conditions below the rain line were poor. A stout crust will be around for a while. 

Conditions continue to be highly variable. We are forecasting today for the most unstable spots in the forecast area. Pockets of more stability may exist, however, the extent of the wind, loading, and number of natural avalanches observed yesterday warrant a cautious rating. It will take a couple of days to see what the extent of the natural avalanche cycle was and how the snowpack throughout the forecast area is responding to the new load. During that time it is wise to recreate on lower angle slopes.

There was a lot of variance in what the storm produced. Yesterday in Crystal Amphitheater, 6″ of wet snow, capped with a crust, sat on top of the old snow. Under the new snow, surface hoar was still present and reactive in compression tests but the overlying slab was not stiff enough to propagate yet. Below this the snow was dry, moisture had not inundated the snowpack despite rain to 7400′.  In Bass Creek, at 7000′, the snowpack was saturated to the ground and without evidence of natural avalanches. On the west side of the Bitterroot Crest, a widespread natural avalanche cycle had occurred. Windslab was failing naturally and propagating long distances, wrapping around terrain features. 

In many areas, where the snowpack was saturated, persistent weak layers should stabilize with freezing. In others where the water did not penetrate the snowpack, persistent weak layers may continue to be an issue. Surface hoar from before this storm could still be lurking and reactive both above and below the rain line. What this means is you need to be heads up. Slight changes of aspect and elevation can still result in drastically different snowpack and stability. One pit and stability test will not suffice to give you a good handle on problem layers. The best way to deal with the myriad of current problems is to investigate the snowpack often. 

Windslab is the biggest concern at higher elevations where abundant new snow is available for transport and there have been 48hrs of sustained wind.

The Bottom Line

Dangerous avalanche conditions exist, travel in avalanche terrain is not recommended. The snowpack has been rapidly loaded and how it is reacting throughout the forecast area is not yet clear. It’s best to give it a couple of days after this storm to settle out. It is certain to trigger wind slabs in steep upper elevation terrain. Avoid wind loaded slopes higher than 7000′. Travel one at a time in avalanche terrain, carry a beacon, shovel, and probe. Remember to reassess conditions throughout the day and stay alert for signs of instability. Dig a pit. Look for red flags.

Upcoming Education Events:

Please visit our education page for an up to date list of regional educational events and course offerings. Below are a few select events and opportunities to check out.

Public Observations

Thank you to everyone who has taken the time to send in a public observation. Please keep sharing what you find and see while out in the backcountry. This online forum is a great resource to glean information about current conditions.

Remember, you can submit your observations through the observation page anonymously. When submitted anonymously, the forecasters review the observation and utilize it when generating the forecast. The information does not appear on the public observation page. 

Ski and ride safe.

 

READ FULL ADVISORY  

Problem 1 - Wind Slab

  • TYPE

    wind-slabs

    Wind Slabs

    Release of a cohesive layer of snow (a slab) formed by the wind.  Wind typically erodes 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.

  • SIZE

    3-4

    1-2 (Small-Large)

    The potential size of avalanche resulting from this problem.

  • LIKELIHOOD

    Likelihood-8

    Very Likely/Certain

    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
    NW - Northwest

We have had 48 hours of sustained wind. Above 7000′ abundant new snow is available for transport. Wind speeds last night were prime for transporting snow.

Strong to extreme winds during the storm transported snow long distances and extensive natural avalanches were failing lower on slopes than normal as a result. Keep this in mind while traveling today.

Leeward and cross loaded slopes have dangerous windslab. Natural avalanches are likely and human triggered avalanches are certain.

Avoid wind loaded slopes over 30 degrees and give a wide berth to run out zones.

Problem 2 - Persistent slabs

  • 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

    4-5

    2 (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

Faceted layers can be found throughout the forecast area. How these were affected by the rain is dependent on how saturated the snowpack became. This is variable. Where saturation occurred freezing temps may heal persistent weak layers. In other areas, these may still be present.

Extensive surface hoar from before the storm may still be an issue, especially above the rain line.

Digging pits is the way to find out if these layers exist. The extended column test (ECT) and the propagation saw test (PST) are best for assessing the stability of these layers. The reactivity of the buried surface hoar can be checked by jumping on small rollovers and pillows, watch for shooting cracks, slab movement, and whumping.

Where faceted layers are found avoid slopes over 30º.

FORECAST & OUTLOOK

Significantly quieter weather will be over the area today and tonight. A quick moving, weak weather system will brush across WC Montana and produce some light snowfall Friday afternoon/evening. Saturday looks to be quite nice across the region, but snow returns yet again on Sunday. This time with better chances for several inches of fresh snow in the terrain.

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.