Avalanche Forecast

Issued: Dec 18th, 2019 10:09AM

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

Northwest Avalanche Center NWAC, Northwest Avalanche Center

Email

Avalanche danger is on the rise. You can trigger avalanches where more than 6" of new snow accumulates and becomes cohesive through wind drifting. Use caution on steep slopes, especially near ridgetops and wind exposed features at upper elevations. With a strong warm front poised to arrive by nightfall, expect very dangerous conditions to develop overnight Thursday into Friday. 

Summary

Discussion

The biggest storm so far this winter is knocking on our doors. Wednesday night into Thursday is the first wave of snowfall, which will be accompanied by winds strong enough to drift the new snow around and create isolated areas of instability. The snowpack is thin, and these cold temperatures have weakened the snow surfaces throughout the zone. Observers have noted these weak snow surfaces. On Tuesday near Blewett Pass I found 5 to 10 inches of soft, faceted snow resting over a stout melt freeze crust. Not a great structure to support the load from a big incoming storm. If you get out, take note on what kind of snowpack structure you find. Is there strong snow over weak snow? How is the new snow bonding to old surfaces? As always, let us know what you find out there.

Very dangerous avalanche conditions look to develop for the area overnight Thursday into Friday with heavy snowfall, strong winds, and a substantial rise in temperatures. Thursday is not a great day to hang it out there and go big. It would be wise to make it back to the vehicle and get things buttoned up by the end of the day. 

Snowpack Discussion

December 12th, 2019 (The regional synopsis is updated every Thursday @ 6 pm)

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

Look for fresh slabs to form during the day as wind transports new snow on exposed upper elevation features. Be especially cautious near gullies and on slopes below ridgelines. You can trigger these slabs where thicker, wind drifted snow rests atop softer snow. Look for signs of instability like shooting cracks, hollow sounding slabs, or recent slab avalanches. Use small hand pits to help evaluate how the new snow is bonding to the old surface. Use small test slopes to check how these fresh drifts may react to the weight of a person or a sled. 

If you find reactive slabs, use caution on slopes over 35 degrees. Avoid steep, unsupported, or obvious wind loaded slopes near and above treeline. Use more supported and lower angled slopes for travel to avoid these areas.

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, Treeline.

Likelihood

Possible

Expected Size

1 - 1

Valid until: Dec 19th, 2019 10:09AM