Avalanche Forecast

Issued: Feb 5th, 2019 10:00AM

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

Calm, cold weather is allowing the snowpack to slowly gain strength. That doesn’t mean you can’t find a lingering wind slab at higher elevations. You are most likely to trigger an avalanche near convex rollovers, on unsupported slopes, or in complex terrain.

Summary

Discussion

Snow and Avalanche Discussion

Observations from the Mt Baker backcountry indicate the snowpack is gaining strength. We received reports of a few human triggered avalanches from Monday and Tuesday. These small slabs triggered on steep convex rollovers near and above treeline.

In shaded and sheltered locations the surface snow is unconsolidated. Cold temperatures and light winds will keep the snow that way for at least the next few days. That means you may trigger small loose avalanches on slopes over 35 degrees. While these sluffs should be small, don’t let them catch you off guard if you are traveling in very steep or high consequence terrain.

If the sun comes out, you may find that the surface snow on steep southerly slopes becomes moist and unstable. You’re most likely to see this on rocky slopes receiving several hours of direct sun. When this occurs, you may be able to trigger small loose wet avalanches on similar slopes.

Snowpack Discussion

February 5, 2019

The active weather pattern this past weekend brought most areas a shot of new snow. Sadly, it seems like areas close to Seattle may have gotten more snow than the mountains. As a result, we are generally finding lower avalanche danger in most of our forecast zones. The general exception to this rule is the mountains closest to the Canadian border. The Baker area received 4” of water since January 31st. Here are a few general trends we see at this point.

The surface is where it’s at:

A combination of high elevation rains in January, a week of warm high pressure, and minimal new snow loads allowed most of our snowpacks to gain strength. In many locations, we are finding that proverbial Cascade “brick.” It’s not that you can’t find any weak snow in the mid- and lower snowpacks, but as a general rule, the snowpacks in our forecast regions are strong. Consequently, most unstable snow will be limited to the snow surface and the last interface buried in the most recent storm. For example, this week observers are primarily tracking the snow surface and the interface buried on February 1st or 3rd, depending on your location.

Very strong surface snow. This crust was buried in most locations Feb 1 or 3. Photo: Chip Daly

How can you use this? Keep your eyes open as you travel and look for areas that appear different. Why are they different? Could this be a rogue wind slab? Is the sun affecting the snow in this location more than other areas? Is the snowpack thinner and weaker in this area? When you find unique areas, it may be worth giving them a wide berth.

Still watching the far-east:

There is a lingering exception… areas east of highway 97 and east-slopes nearer to the Columbia River. As you travel further east in our forecast area, the snowpack gets thinner, weaker, and more variable. So, why are we seeing the avalanche danger go down in these locations? In general, there just isn’t a substantial slab over the buried weak layers. Two things could change that. 1. A wind event. One quick way to get a slab is to build one with some dry snow and moderate winds. That’s why we have wind affected areas on our mind when we travel to areas with thinner snowpacks. 2. A big storm. While areas like the Wenatchee mountains have seen their fair share of snow this season, these areas haven’t seen a big loading event. How would this weak snowpack handle a big storm? It’s hard to say at the moment. Just remember, if you go to mountainous areas around Twisp, the Wenatchee Mountains, or the East-South zone, you may encounter snowpacks with lingering persistent weak layers.

A shovel tilt test highlights weak snow interfaces in a very shallow east-side snowpack. Photo: Josh Hirshberg

The danger is real:

Even though the snowpack is strong and the avalanche hazard is generally low, there are other risks in the mountains that may pose a very real danger to backcountry travelers. The one we keep hearing the most about is very firm and slick surfaces. You are most likely to find icy surfaces in locations that did not receive much snow during this recent storm. When conditions are like this, it’s tough to gain traction, and any slip may result in a long uncontrolled fall.

Icy snow surfaces have been making travel conditions difficult, and sometimes dangerous. This firm, slick layer is buried below the most recent snow in many locations. Photo: Dallas Glass

What’s next?:

Given the strength of the snowpack, it will likely take a larger storm to ramp the avalanche danger back up. When will that storm arrive? We’ll keep watching the weather patterns and let you know. Make sure to check the latest weather and avalanche forecast before you head into the mountains.

-NWAC team

Problems

Wind Slabs

An icon showing Wind Slabs

The wind slabs are now a few days old. This should mean they are more difficult to trigger. When we get into situations like this, we start thinking about slope features where it is easier to trigger an avalanche. You are most likely to trigger a lingering wind slab near convex rollovers, on unsupported slopes, or in more complex terrain. You’re more likely to find old wind slabs at higher elevations, and in areas that are more prone to wind, such as near ridges and passes. Keep your eyes open as you travel, and take a moment to identify slope scale features you want to avoid.

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: Feb 6th, 2019 10:00AM