Posted:
Jan 28, 2021 @ 6:45 am

The avalanche danger is Moderate in the Rattlesnake and LOW in the central and southern Bitterroot, and Seeley Lake zone. It is possible to trigger an avalanche in the Rattlesnake. There are isolated avalanche problems in the other zones. Low does not mean no avalanche danger.

Good Morning. This is Jeff Carty with the West Central Montana Avalanche Center advisory on Thursday, January 28th, 2021. This advisory is sponsored by the Rocky Mountaineers. This advisory does not apply to operating ski areas and expires at midnight tonight. The USDA Forest Service is solely responsible for its content.

Weather and Snowpack

Mountain temperatures range from 18º to 28º F this morning. Some areas in the Bitterroot picked up 0.1″-0.3″ SWE in the last 24h. Winds are southerly and light with moderate gusts, blowing harder at ridge top in the Swans.

Not much has changed throughout the forecast area. Surface hoar and near surface facets have developed and will be an issue if we get a load of snow on top of them. The wind picked up a bit and transported snow to leeward aspects.

Low hazard is defined as: Generally safe avalanche danger, watch for unstable snow on isolated terrain features.

This is what we have throughout the majority of our forecast area. Overall it is unlikely to trigger an avalanche. However, due to spatial variability, isolated instabilities are present. Diligent hazard assessment is required despite the low rating. Suspect areas are shallow snowpacks, generally under 4 feet in depth, where persistent weak layers exist. These can be found at mid elevations and on wind scoured slopes. Upper elevation leeward slopes may contain wind slab. Cornices have been growing and are a hazard. Terrain traps will increase the consequences of these problems.

The exception to the low rating is the Rattlesnake, where there is moderate hazard. This range has received less snow than the rest of the forecast area and as a result, the structure has been slowly deteriorating due to the growth of facets and depth hoar. These layers are stubborn and deep. We were still finding propagation on multiple layers yesterday in the Rattlesnake, indicating that the problem is not going away. See this video. While it is not likely to trigger these layers, it is possible. Given the depth and stiffness of the slab, the resulting avalanche could be very destructive. 

Layers such as this can be tricky to assess. As persistent weak layers get buried deeper, they become unpredictable. They will likely not give warning signs such as cracking or whumphing, can avalanche despite being skied repeatedly, and as they get deeper can produce false stable results on extended column tests. The propagation saw test is a good test for deep faceted layers if you are not seeing propagation in the ECT. The best approach is to avoid slopes over 30º. 

Bottom Line

Generally stable conditions exist, except in the Rattlesnake where it is possible to trigger an avalanche. Due to spatial variability, isolated instabilities are present throughout the forecast area. Avoid slopes with weak sugary snow. Do multiple pits investigating the stripes in your pit wall. Avoid cornices and wind loaded terrain. Choose simple terrain that does not expose you to terrain traps. Avoid likely trigger points on slopes.

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.

You can now text us your observations to (406) 219-5566 when you don’t have time to fill out the observations page. Texted observations won’t get posted on the website, but will be used in the development of the forecast.

Ski and ride safe.

 

READ FULL ADVISORY  

Problem 1 - Persistent weak layers

  • 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

    5-6

    2-3 (Large)

    The potential size of avalanche resulting from this problem.

  • LIKELIHOOD

    Likelihood-3

    Possible

    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. Shallower snowpacks have worse structure than deeper areas and are more suspect. In some places, persistent slabs are up to 40 inches thick and have become low likelihood, high consequence problems. The worst faceting is in the Rattlesnake where depth hoar has developed at the base of the snowpack, especially on shaded, northerly aspects.

Look for soft sugary snow as you assess the snowpack.

The rain crust from 01/13/2021 has facets below but has been gaining strength. Located from the surface to 1 foot deep in the snowpack depending on location. It can be found up to 8500 ft in some areas.

Surface hoar has developed in most areas, and near surface facets are developing with the cold nights. While not currently a problem these will become weak layers when buried.

The extended column test (ECT) and the propagation saw test (PST) are best for assessing the stability of the persistent weak layers.

Problem 2 - Wind slab and cornice fall

  • 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

    2-3

    1 (Small)

    The potential size of avalanche resulting from this problem.

  • LIKELIHOOD

    Likelihood-3

    Possible

    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

Winds rose to moderate yesterday transporting snow to leeward slopes, wind slab was building.

Upper elevations, just below ridgeline are where these are most likely found.

Watch for pillows and drift like formations. Shooting cracks are a warning sign.

Carefully assess wind loaded start zones and cross-loaded slopes greater than 35º.

Stay out from underneath cornices, and well away from the top.

VIDEO

FORECAST & OUTLOOK

Weak waves will bring off and on snow showers over the next 24 hours in the Bitterroot Mountains mainly. Don’t expect to pick up more than an inch or two of accumulation and it will be spotty at best. A slightly more organized wave could bring a better chance for snow on Friday, again mainly for the Bitterroots, but locations towards the Rattlesnake region could also pick up a light dusting. Snow showers persist into Saturday with mild conditions. Milder than average temperatures with mainly dry conditions are expected Sunday and Monday.

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.