Posted:
Dec 17, 2020 @ 6:46 am

The avalanche danger in the west central Montana backcountry is a strong Moderate. Isolated pockets of higher hazard may exist.

Good morning, this is Jeff Carty with the West Central Montana Avalanche Center’s avalanche advisory for December 17, 2020. This advisory does not apply to operating ski areas, expires at midnight tonight, and is the sole responsibility of the U.S. Forest Service.

Mountain temperatures are 23º to 32º this morning. 

The Snotel sites tell us the mountains received between 0.3″ and 0.7″ of snow water equivalent in the past 24 hours. Tours yesterday revealed 4-6″ of new snow on the ground at St. Mary’s, 6″ at Glen lake, 3″ at Sheep Mt, and 2″ in the southern Bitterroot around Lost Trail. 

There is a broad range of conditions throughout the forecast area, some areas have touchy windslab, some have a reactive surface hoar layer under the new snow, others are still generally stable. Approach all slopes with suspicion and practice extra caution as the mountains receive more snow and wind.

Tuesday’s snow came in with moderate winds at upper elevations and there was evidence of considerable wind transport yesterday. Further snow and wind last night have added to the thickness and size of wind slabs. These overlay a variety of surfaces including near surface facets and surface hoar compounding the wind slab problem. Yesterday in the Lost trail backcountry wind slabs at ridge top were remotely triggered and some combination of persistent weak grains likely played a role.  Due to the presence of the weak grains wind slabs may remain touchy for longer than normal. All upper elevation, leeward slopes likely have windslab. 

Buried surface hoar can be found throughout the forecast area. In many places, the overlying slab lacks the cohesion or depth to propagate. However, it was very reactive, failing on isolation on a NE slope at 7300′ on Sheep Mt yesterday and woomfing was experienced. In the Rattlesnake, 6″ of storm snow was failing easily on surface hoar and there were rumors of cracking and shifting snow on Mt. Fuji at Lolo Pass where widespread surface hoar was noted. Lolo Pass received the most snow last night, roughly 7″, bringing the storm total to over 12″ so far, and creating the thickest slab over this problem layer in the forecast area. Practice extra caution if you are riding there today.  As more snow accumulates throughout the forecast area this could become a widespread problem. 

Most areas are also plagued by faceting deep in the snowpack, which has continued to lose cohesiveness. These layers are not yet propagating consistently in stability tests but the structure is very poor.  Observations yesterday indicated these facets are continuing to grow. The snowpack on sheep Mt. was considerably more faceted than 2 weeks ago. The snowpack on NW slopes on Pyramid peak is composed entirely of noncohesive facets, reminiscent of our snowpack leading up to the January avalanche cycle last year. The concern is that as snow piles up as a cohesive slab over these weak layers it may trigger a large avalanche cycle. With snow in the forecast throughout the week, high winds, increased temps, and abundant moisture forecast this weekend we may see the avalanche hazard rise sharply. 

The Bottom Line:

Winds have created touchy windslab that will continue to grow with snow and wind today. Avoid wind loaded start zones greater than 30º. A variety of persistent weak layers exist throughout the snowpack which is currently being loaded by new snow. Storm snow failing on buried surface hoar is possible, with more risk in areas that received more snow.  The likelihood of avalanches will increase with continued snowfall.  As always practice safe travel protocols. Travel one at a time in avalanche terrain, carry a beacon, shovel, and probe, and stay alert for signs of instability. Dig a pit. Look for red flags

The current storm cycle coincides with the start of the holidays and we expect to see more people out in the backcountry in the coming week. Please exercise caution. We are coming out of a long stretch of low hazard and no snow, the draw of fresh powder is strong but we may be entering into a very active avalanche cycle. 

We generate avalanche forecasts for a 1420 square mile area that stretches from Lost Trail Pass to just north of Seeley Lake. We work hard to keep you informed of current avalanche dangers but, we can’t see everything. Your snowpack and weather observations help us fill in the gaps and produce a more accurate forecast. If you get out, please take a moment to fill out the online observation form

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

    2-3

    1 (Small)

    The potential size of avalanche resulting from this problem.

  • LIKELIHOOD

    Likelihood-5

    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

Wind slabs are present and growing on upper elevation slopes.

In places these are touchy and it is possible to trigger an avalanche that could bury a person.

Watch for stiff, hollow-sounding snow, wind loaded pillows, and shooting cracks.

Avoid wind loaded start zones greater than 30º.

Problem 2 - Persistent slab

  • 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

    3-4

    1-2 (Small-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

A variety of persistent weak layers exist in the snowpack.

The ones most likely to fail currently are buried surface hoar and near surface facets.

These are touchy in some spots and unreactive in others. It is possible to trigger avalanches on this layer. As the new snow builds depth and consolidates these layers are more likely to fail and propagate to larger areas.

Watch for shooting cracks and woomfing. Perform stability tests before venturing onto slopes greater than 30º

Also of concern are faceted layers deeper in the snowpack. As snow depths increase these will be stressed further. A challenge with deeper persistent weak layers is that they are unpredictable. Continued snow load and warming temps this weekend may stress layers to the point of failure or it may not. As the snow piles up more it’s best to avoid steeper slopes and obvious avalanche paths until we know how these layers will react.

VIDEO

Observation Sheep Mountain 12/16/2020

FORECAST & OUTLOOK

Snow showers will continue through Thursday night. A quick hitting weather system is expected Friday night bringing the potential for many inches of snow and increased westerly winds through Saturday morning. The atmospheric river is still on track to arrive Saturday night. Gusty southwesterly and westerly winds may gust over 50 mph. Snow levels are expected to rise to around 5000 feet during Sunday. Liquid water content between Saturday night and Sunday night could range from 1.00-2.00 inches in the Bitterroot Range and around an inch elsewhere. Another wet system is possible early next week, likely with lower snow levels.

 

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.