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 Storm Slabs.

Northwest Avalanche Center NWAC, Northwest Avalanche Center

There is a lingering chance of triggering avalanches 1-2ft deep at upper elevations. Give the snowpack time to adjust before pushing into complex alpine terrain and steep unsupported slopes. Even a small avalanche could have high consequences in these shallow, early season conditions.

Summary

Discussion

In the past week, the Mt. Baker area received over 3ft of new snow (3.25in water) above 4000ft. The bulk of precipitation fell on Thursday and Friday. Intermittent snowfall and light southerly winds continued through Saturday, with clearing and periods of sunshine on Sunday. Expect a slight chance for light snow showers and mostly cloudy skies Monday and Tuesday before a series of weather systems impact western Washington later in the week.

The recent storm dramatically improved snow cover, and brought the first round of notable avalanche activity. Several small avalanches (D1.5) were triggered by skiers and riders in the Hwy 542 corridor over the past few days. The majority of these avalanches failed on the old/new snow interface about 2ft deep, while some failed within new snow about 1ft deep. These avalanches occurred on north and east aspects above 5500ft on unsupported slopes steeper than 35 degrees. No natural avalanches were reported. Below 5000ft, the recent snow fell on sparse snow cover and mostly bare ground. Travel at lower elevations is challenging with plenty of shallowly buried obstacles.

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

Storm Slabs

An icon showing Storm Slabs

You are most likely to trigger a storm slab avalanche above 5500ft, primarily on north and east aspects. These avalanches could break about 2ft deep on the old/new snow interface buried earlier in the week on 12/10/19, or within the new snow. The old/new snow interface is variable, and in some upper elevation areas, harbors weak snow (rounding facets/surface hoar). However, a lack of recent natural avalanche activity and favorable snowpack test results indicate that it is gaining strength. Below 5000ft, triggering an avalanche is unlikely as the recent snow bonded well to sparse old snow cover and bare ground. Carefully evaluate how the recent snow is bonding to itself and old snow surfaces. Be leery of unsupported slopes, wind drifted snow, and large terrain features steeper than 35 degrees at upper elevations.

Release of a soft cohesive layer (a slab) of new snow that breaks within the storm snow or on the old snow surface. Storm-slab problems typically last between a few hours and few days. Storm-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.

 

You can reduce your risk from Storm Slabs by waiting a day or two after a storm before venturing into steep terrain. Storm slabs are most dangerous on slopes with terrain traps, such as timber, gullies, over cliffs, or terrain features that make it difficult for a rider to escape off the side.

 

Storm slabs usually stabilize within a few days, and release at or below the trigger point. They exist throughout the terrain, and can be avoided by waiting for the storm snow to stabilize.

Aspects: All aspects.

Elevations: Alpine, Treeline.

Likelihood

Possible

Expected Size

1 - 1

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