Posted:
Jan 7, 2020 @ 7:07 am

The avalanche danger for the west central Montana backcountry is HIGH on all slopes over 5500 feet in elevation. All other slopes the danger is CONSIDERABLE. New snow and winds are creating large dangerous avalanches. Travel in avalanche terrain is not recommended. 

Good morning, this is Travis Craft with the West Central Montana Avalanche Center’s avalanche advisory for January 7, 2019. 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

Mountain temperatures range from 26F to 33 F in the region. In the Bitterroot, winds are 7 mph with gusts of 17 out of the S. In the northern part of the advisory area, winds are 16 mph and gusting 27 mph out of the SW. Snotels are reporting between .6 and 2.1 inches of SWE for the last 24 hours for 6 to 12 inches of new snow.

Yesterday a system of subtropical moisture entered the forecast area. Winds scoured many slopes over the weekend. The new snow from this system is loading leeward slopes and creating very dangerous avalanche conditions. Yesterday, Jeff and I were getting shooting cracks on wind loaded slopes. Overnight with the additional loading of snow, these wind slabs will be larger and more easily triggered. 

The new snow is falling on a poor snowpack structure that has the potential to create large avalanches. We are still getting propagations in our stability tests on the buried surface hoar crust combinations and a layer of depth hoar. The new snow will make these layers more sensitive today.

The primary avalanche problem today is persistent slabs. There are two layers of concern in our snowpack, a layer of surface hoar and near-surface facets below a thin crust that the New Year’s storm buried about 2 to 3 feet deep. This layer failed several times,  producing both natural and human triggered avalanches during the New Years’ cycle. The other is a layer of facets or depth hoar below a crust near the bottom of our snowpack. We are still getting these to fail in stability tests. There is the possibility of triggering the whole season’s snowpack in a very large slide on this layer near the ground.

The second avalanche problem is wind slabs. Leeward slopes have been loaded and are easily triggered. Identify wind loaded terrain and avoid traveling on or below these slopes today.

The third avalanche problem is new snow. Trigging storm slabs that step down into deeper buried weak layers today is possible. Avoid slopes over 30 degrees. 

Bottom line: There are very dangerous avalanche conditions today. Do not travel on or below wind loaded terrain. Travel in avalanche terrain is not recommended. Stick to lower angled sheltered slopes that are not connected to steep terrain because it is possible to trigger our buried weak layers remotely from the side, below, or  above. The buried weak layers in our snowpack have the potential to create large dangerous avalanches, proof of this comes from observations of the natural and human triggered slides over New Years and the weekend(see public observations and report). Everyone in your group should have a beacon, shovel, and probe. Only one person on a slope at a time. 

Avalanche and Weather Outlook

More snow and rising temperatures predicted today. Watch out for red flags such as cracking, collapsing, and recent avalanches. The avalanche danger will rise throughout the day with wind and more snow. See the forecast.

 Thank you to everyone who has been sending in public observations. As always, if you make it out, please, feel free to share what you find on our public observations page.

Ski and ride safe.

 

READ FULL ADVISORY  

Problem 1 - 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

    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.

Recent avalanches and snow pit test results confirm that we have a persistent slab avalanche problem.

It is possible to remotely trigger avalanches within this layer from below, above or adjacent to an avalanche slope, on low angle terrain (>30º). The friction is very low (slippery), and slopes that would not normally slide may be able to. Be very critical and suspect of all slopes over 30º.

Problem 2 - Wind Slabs

  • 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-7

    Very Likely

    The likelihood of an avalanche resulting from this problem.

Remember even a small wind slab has the potential to step down creating a larger persistent slab avalanche.

Problem 3 - New Snow

  • 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

    3-4

    1-2 (Small-Large)

    The potential size of avalanche resulting from this problem.

  • LIKELIHOOD

    Likelihood-5

    Likely

    The likelihood of an avalanche resulting from this problem.

Even a small storm slab has the potential to step down into deeper layers of our snowpack.

VIDEO

Observations 01/06/2020

Observations for January 07, Advisory.

FORECAST & OUTLOOK

New snow and wind will increase the avalanche danger. See the forecast.

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.