Avalanche Forecast

Issued: Jan 19th, 2018 10:35PM

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

Northwest Avalanche Center NWAC, Northwest Avalanche Center

Deep areas of wind and storm slabs should make triggering an avalanche in steep terrain possible or even likely. Avoid travel on steep slopes receiving wind deposited snow, where fresh wind slab deposits will be sensitive to human triggering. Expect dangerous avalanche conditions at higher elevations.  Choose conservative terrain, by travelling in wind sheltered terrain well away from avalanche paths.

Summary

Detailed Forecast

A band of enhanced snow showers should arrive Friday night with diminishing showers Saturday. This should freshen storm snow with winds continuing to redistribute new cold snow to lee slopes by Saturday. 

This weather should cause widely variable snow conditions with some wind exposed slopes scoured to recent crusts and lee slopes building deeper wind drifts and slabs. Watch for changes in snow conditions, particularly stiffer more dense snow, likely a wind or storm slab. Avoid travel on slopes if you encounter wind stiffened surface snow, especially on steeper exposed terrain and steep roll-overs.  

The temperatures should remain cool, depositing new low density snow that will be easy for winds to re-distribute on exposed terrain.  

Wind slabs near and above treeline remain the primary avalanche problem in this area, so remain conservative in your terrain choices especially as you venture into exposed terrain.

The best and safest snow will remain in sheltered terrain away from ridges. 

Snowpack Discussion

New storm snow amounts vary according to elevation as rain gradually changed to snow Wednesday night. By Friday, storm snow ranges from about 6-8 inches in lower terrain and 16-24 inches in higher elevation terrain. 

Above treeline, greater new snow amounts and periods of very strong winds have caused dangerous avalanche conditions. New wind and storm slabs in higher exposed terrain will require careful terrain choices and conservative decision making.  

Near and below treeline the precipitation began as rain and transitioned to snow. This has caused less dangerous conditions with new snow forming good bonding to the old rain soaked snowpack. However, heavy snowfall and moderate to strong winds have built increasing wind and storm slabs at progressively lower elevations. There are still heightened avalanche conditions with new and increasingly deep wind and storm slabs of 1-2 ft or more as of Friday.

The old rain wet snow continues to gradually re-freeze and form a new crust layer.

The older snowpack has undergone several rain or warm periods and remains void of any significant layers of concern.

Observations

North

On Friday, professionals for NWAC traveled to near treeline and avoided higher exposed terrain above treeline due to potential for large and dangerous wind slabs. Takeaway was the active wind transport and new snow happening throughout the day as well as evidence of significant recent wind re-distribution of the deep storm snow. Most slabs encountered were shallow, soft slabs formed from wind loading. There was evidence of a large wind slab release above treeline on a north aspect with a depth roughly estimated at 3 ft or more.   Up to treeline there was about 2-3 ft of storm snow over the forming Jan 16 rain crust.

Thursday morning, the Mt Baker Pro Patrol reported fresh wind slabs were sensitive to ski cuts and were releasing in the 4-5 inch range, near treeline. Winds were reportedly very strong along ridges and actively transporting the new snow. 

Thursday morning, the Mt Baker Pro Patrol reported fresh wind slabs were sensitive to ski cuts and were releasing in the 4-5 inch range, near treeline. Winds were reportedly very strong along ridges and actively transporting the new snow. 

Central

NWAC staff traveled in the Alpental Valley Friday, finding highly variable storm snow conditions due to the active and ongoing wind transport of the recent storm snow. Some exposed slopes were striped of new snow to firm crust layers with nearby slopes holding over 2 ft of wind deposited snow. Bonding to old wet snow was good. The forming rain crust was ski supportable above 5000 ft but remained soft and breakable below 5000 feet. 

NWAC forecaster, Dallas Glass was on Skyline Ridge at Stevens Pass Thursday and reported new storm snow of 8 inches at 4000 feet and 14 inches above 5000 feet. The bonding was good to the old rain wet snow. The crust had yet to re-freeze but was in the process. There was evidence of recent wind transport with a fresh natural avalanche having released on a steep east face about 5300 feet, likely during a brief warm up Wednesday night. There were storm slab layers noted from fluctuating temperatures overnight, but were not sensitive to human trigger in that location. 

South

On Friday, NWAC forecaster Dallas Glass traveled in the Crystal Mountain back country from 4200-6600 ft covering all aspects. The recent winds have caused highly variable storm snow conditions with exposed areas striped of recent snow and more wind loaded N-NE aspects holding up to 6 ft of storm snow! There was a lack of storm slab in wind sheltered terrain with widely varied wind deposited snow near treeline exposed to recent strong winds. 

Pro Patrol at Crystal Mountain Thursday morning reported shallow 2-4" very soft slabs were sensitive to ski triggers on control. These slabs were breaking up and running as very soft slabs and were generally shallow. The underlying rain crust have become very firm by Thursday morning above 6000 ft and gradually softer at lower elevations.

Problems

Wind Slabs

An icon showing Wind Slabs

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: North, North East, East, South East, North West.

Elevations: Alpine, Treeline.

Likelihood

Likely

Expected Size

1 - 1

Storm Slabs

An icon showing Storm Slabs

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: All elevations.

Likelihood

Possible

Expected Size

1 - 1

Valid until: Jan 20th, 2018 10:35PM