Avalanche Forecast

Issued: Dec 15th, 2019 10:00AM

The alpine rating is moderate, the treeline rating is low, and the below treeline rating is low. Known problems include Wind Slabs.

Northwest Avalanche Center NWAC, Northwest Avalanche Center

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At upper elevations, you could trigger avalanches that were formed by gusty wind and snow late last week. The avalanche danger is most elevated in the Wenatchee Mountains and on the highest slopes in the range. When sliding and riding below treeline, watch for travel hazards is due to low snow cover such as shallowly buried rocks, stumps, and creeks.

Summary

Discussion

Over the weekend, observers at Mission Ridge reported signs of instability such as collapses, cracks shooting through the snow, and avalanches on leeward and cross-loaded slopes. On Sunday, an observer in the Teanaway drainage reported small loose wet avalanches on the south face of Fortune Peak and 1-1.5 feet of recent storm snow since December 10th. You may find persistent weak layers immediately below the storm snow and possibly in the lower half of the snowpack.

Travel hazards such as shallowly buried rocks, stumps, and logs exist. Be cautious when traveling in the backcountry due to shallow cover. Observations have been limited and there is still a good bit of uncertainty about conditions. Be prepared to make your own observations and snowpack assessments. Let us know what you see in the mountains!

Snowpack Discussion

December 12, 2019

After a dry November, this week marks the beginning of more winterlike weather across the region with snow at middle and pass level elevations. While there’s uncertainty in the weather forecast, it does appear that the snowpack will continue to build to some extent over the coming week. 

Throughout much of the region, the slow start to winter has left avalanche conditions distinctly defined by elevation. Slopes above 5,500-6,000ft hold a layered snowpack that provides enough coverage for winter travel and avalanches. Below this elevation, most slopes were bare until the past week. At these lower elevations, it will likely take another round of storms before larger avalanches are possible and travel becomes easier.

 

Image courtesy of the Natural Resources Conservation Services interactive map showing Snotel weather stations measuring well below normal snow water equivalent for this season so far.

 

Upper Elevations

The lack of significant snowfall has resulted in commonalities throughout the region. Slopes above about 5,500ft currently hold the ”deepest” snow cover and the most layered snowpack. Until the lower elevation terrain builds a more substantial snowpack, the upper elevations will hold the most potential for producing large avalanches. If you dig into the snow in these areas, you’ll find a range of height of snow and a variety of layers. Here are a few layers to note:

  • The interface of older snow and any new incoming snow would be the first interface to check.

  • Snowfall around December 7th and 11th may have buried surface hoar and near-surface facets in some locations. As of Dec 12th, these interfaces can be found 1-2’ below the surface.

  • A layer of facets can be found near the middle of the snowpack, buried just before Thanksgiving. Where found, the facets are often rounded or have even undergone some melt-freeze metamorphism from liquid water.

While these layers give you something to look at in snow profiles, they may not be your main snowpack concern for the day. Continue to check the daily zone forecasts for the most up to date avalanche conditions. We’ll monitor these layers as future weather brings changes to the snow and avalanche conditions.

 

A layer of facets in the middle of the snowpack resulted in sudden test results on Dec 11th. Rock Mtn, N, 6270ft. Photo: Josh Hirshberg.

 

Middle and Lower Elevations

At most locations below 5,500ft, slopes are still building uniform snow cover. In many zones, the hazard of hitting rocks or shallowly buried objects may be more significant than the avalanche danger. Depending on future weather, the snowpack could continue to form or could, unfortunately, melt out to the ground. While there’s little layering of note at these elevations, avalanches aren’t completely out of the question with the right weather input. Further low elevation snowfall or warming could drive avalanche activity. The East North forecast zone, including Washington Pass, has more low elevation snow than other zones and therefore more potential for avalanches at these elevations. As with the upper elevations, we’ll wait and see what the next round of weather brings.

Problems

Wind Slabs

An icon showing Wind Slabs

You can trigger avalanches in freshly formed drifts and areas where you find stiffer wind-blown snow sitting on older snow. These avalanches are sticking around longer than usual due to a layer of facets that were buried on December 10th. Watch for “red flag” warning signs like cracks shooting through the snow or whumpfing collapses. Steer around obvious wind features and pillows on leeward sides of ridges and cross-loaded terrain. Use caution on slopes over 35 degrees, where you find 6 inches or more of drifted snow. Check the bond between the recent slabs near the surfaces and older snow. Use small, inconsequential test slopes to check if you could trigger an avalanche. When in doubt, defer to lower-angled terrain.

Avalanche conditions will be most dangerous where the strong and gusty wind drifted the recent snow at upper elevations, especially in the Wenatchee Mountains and the eastern portion of the forecast zone. If the sun comes out, you may encounter small point release avalanches on sun-exposed slopes.

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

 

Wind Slabs form in specific areas, and are confined to lee and cross-loaded terrain features. They can be avoided by sticking to sheltered or wind-scoured areas..

 

Wind Slab avalanche. Winds blew from left to right. The area above the ridge has been scoured, and the snow drifted into a wind slab on the slope below.

 

Wind slabs can take up to a week to stabilize. They are confined to lee and cross-loaded terrain features and can be avoided by sticking to sheltered or wind scoured areas.

Aspects: All aspects.

Elevations: Alpine.

Likelihood

Possible

Expected Size

1 - 1

Valid until: Dec 16th, 2019 10:00AM