Avalanche Forecast
Regions: Cascades - South West.
New snow and wind will create dangerous avalanche conditions Saturday. You can trigger an avalanche on any steep wind loaded slope. Moderate easterly winds will load unusual aspects and build wind slabs on open slopes below treeline as well as higher terrain. In wind sheltered areas, loose dry avalanches can run fast and far, don't let them catch you off guard. Storm slabs may also be found in steep terrain below treeline.
Discussion
Snow and Avalanche Discussion
Change is in the air as cold dry snow is forecast to pile up Friday night and Saturday morning. Avalanche conditions should quickly become dicey and dangerous on Saturday because the new snow comes with a catch; moderate east winds that will easily transport new and old snow onto unusual aspect and a variety of weak snow surfaces.Â
In non-wind affected terrain, loose dry avalanches will be more likely where the snow stays unconsolidated. And if snowfall rates and totals exceed threshold rates, even soft storm slabs are possible in non-wind affected terrain.Â
With all of this in mind, it will be difficult to manage avalanche conditions Saturday, so stay safe and choose simpler terrain.
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
Avalanche Problems
Wind Slabs
Avoid steep wind loaded slopes in all elevation bands Saturday. New wind slabs may be especially touchy where they build over weaker, older snow surfaces. In addition, moderate easterly winds are expected to build wind slabs on unusual aspects. Low density snowfal will easily be transported onto lee slopes. With all of this in mind, it will be difficult to manage avalanche conditions Saturday, so stay safe and choose simpler terrain.
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: All elevations.
Likelihood: Likely
Expected Size: 1 - 1
Storm Slabs
If storm slabs develop Friday night and Saturday, they may be touchy and break more widely than usual where they build over older, weaker snow. Avoid very steep open slopes and convexities and choose simpler terrain if conditions are touchy. Use small test slopes to gauge the storm slab problem.
Loose dry avalanches will continue to be a concern in very steep terrain that isn't wind affected. Keep this in mind around terrain traps; you don't want a small but fast moving avalanche to take you on an unexpecting ride into trees or over a cliff.
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.
Elevations: Below Treeline.
Likelihood: Possible
Expected Size: 1 - 1