Posted:
Feb 23, 2019 @ 6:16 am

The avalanche danger early this morning is moderate but will shift towards considerable as the day progresses. This morning, human triggered avalanches are possible but will trend towards likely as the new snow stresses the snowpack and new problems develop. Dangerous avalanche conditions will emerge and will require careful snowpack evaluation, cautious route-finding and conservative decision making.

Good morning, this is Logan King with the West Central Montana Avalanche Center’s avalanche advisory for Saturday, February 23rd, 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

Over the last 24 hours, the forecast area has picked up 3 to 6 inches of new low-density snow. The fresh snow has added 0.2-0.5 inches of SWE. Mountain temperatures as of 4 am this morning are in the teens. The winds are 6 mph with gusts up to 16 mph from the SE in the southern Bitterroot and primarily S in the northern region of the advisory area.

Persistent slabs are a significant concern today. A layer of surface hoar is getting buried by the new snow and will become reactive as a slab forms over this weak layer. There are other layers of buried surface hoar that were gaining strength but will be under more stress with the new load of snow. A layer of cold preserved storm snow is still suspect and can be reactive at some locations; this layer is hard to identify but can be found when performing stability tests. Faceted snow has the potential to become more responsive with the new load as does the depth hoar, although it is deep an unlikely to be triggered except in a step-down avalanche.

Winds have mostly been light but ramped up to moderate strength for a few hours yesterday evening. Wind slab development occurs much faster so the small wind slabs likely grew overnight. There is plenty of snow for transport and in areas with more powerful winds look for growing wind slabs. Larger wind slabs are possible in bigger terrain like high elevation bowls and below summit ridges. The variable winds have again made it difficult to identify all terrain that is loaded, and there is a significant amount of cross loaded terrain right now. Be on the lookout for any signs of wind loading and stay aware of conditions as the change through the day today.

Loose snow avalanches will easily be triggered in steep terrain today. The new snow is light and will sluff readily. Avoid terrain traps as they increase the consequences of getting knocked off your feet or sled and going for a ride. The loose surface snow will become more problematic as more snow is added over the weekend and starts to form a slab creating new widespread storm slabs.

Avalanche and Weather Outlook

Snowfall has slowed this morning, but an additional 2-4 inches of low-density snow are expected today. Winds should build and shift to the E-NE and begin to redistribute the new low-density snow. Another round of snow is setting up for tonight into Sunday. With increased wind and snow the avalanche danger will continue to trend upwards.

Bottom Line: A good dose of new snow and strengthening winds will easily push the avalanche danger to considerable. The question is when do the scales tip? Some locations will get there faster than others, either because of more load or due to the freshly buried layer of surface hoar. Stay vigilant in the backcountry today and continue to evaluate conditions as they change, watch for growing signs of instability like collapsing, shooting cracks, whumphing, and natural avalanche activity. Human triggered avalanches will become likely so utilize conservative decision-making to avoid finding the tipping point and getting caught in a slide.

Feel free to share what you find in the backcountry on our Public Observation page. It’s a great resource for us and the whole backcountry community.

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

    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.

Persistent slabs will become more likely as surface hoar gets buried. The deeper layers of BSH and facets will also become more reactive as they become stressed under the new load of snow.

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-3

    Possible

    The likelihood of an avalanche resulting from this problem.

Small to large wind slabs are possible and will be growing in size and sensitivity over the weekend.

Problem 3 - Dry Loose Snow

  • TYPE

    loose-dry

    Loose Dry

    Release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose-Dry Avalanches,they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. They generally move slowly, but can contain enough mass to cause significant damage to trees, cars or buildings. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose-wet avalanches can trigger slab avalanches that break into deeper snow layers.

  • SIZE

    1-2

    < 1 (Small)

    The potential size of avalanche resulting from this problem.

  • LIKELIHOOD

    Likelihood-5

    Likely

    The likelihood of an avalanche resulting from this problem.

Sluffs will be likely today in steep terrain.

VIDEO

FORECAST & OUTLOOK

  • Danger Trend

    increasing

    Increasing Danger

  • Area Forecast

    Snow

Light snow today with another round setting up for Sunday.

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.