Avalanche Forecast

Issued: Jan 21st, 2015 10:00AM

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

Northwest Avalanche Center NWAC, Northwest Avalanche Center

The weather should have limited effects on snow conditions on Thursday. Mainly watch for lingering areas of firmer wind slab on previous lee slopes.

Summary

Detailed Forecast

A weak dissipating front should move through an upper ridge and across the Northwest on Thursday. This should cause some light snow in areas east of the crest with a minor drop in snow levels.

This weather should have limited effects on snow conditions.

Mainly watch for lingering areas of firmer wind transported snow and wind slab on previous lee slopes from the back end of the storm early this week.

New snow amounts should be limited on Thursday and any new wind slab should be unlikely, shallow and small if any.

Loose wet avalanches will not be indicated due to the cloud cover and cooling. Storm slab will also not be listed due to the expected limited amounts of new snow. 

In the Washington Pass area lingering wind slabs releasing down a the January 5th crust/facet interface deserves attention. Watch for cracking and collapsing while traveling as obvious instability clues and generally be conservative near avalanche terrain. There's plenty of good skiing to be found on lower angled slopes even in the alpine. The northeast zone will have a higher danger rating than the other zones east of the crest.

As a general backcountry travel safety note, tread carefully at lower elevations and on wind scoured aspects where terrain hazards (exposed rocks, trees, streams, etc.) are present. 

Snowpack Discussion

Strong southwest flow carried a wet front across the Cascades Saturday night. This front tapped subtropical moisture but cold air trapped on the east side caused water amounts through Monday morning of .5-2 inches to fall mainly as snow. Snow was most significant in the northeast Cascades with about 12-24 inches at Holden and Washington Pass through Monday morning. 

The North Cascade Mountain Guides in the Washington Pass Monday reported storm slab and collapsing down 55-70 cm in 2-3 mm facets on the January 5th crust. This layer was reactive in snowpit tests with extended column tests indicating propagation and one natural R2D2 avalanche in the Cutthroat Drainage that may have released down to this layer.

Storm slab was reported in the Stevens Pass area Monday and this avalanche problem likely extended into the neighboring area along the east slopes.

We have no new information about the non-reactive PWL in the Jove Peak area from last week, but following this storm cycle it is likely more than 1 meter down and even harder for a human to trigger. 

An avalanche class near Mission Ridge on Saturday reported via the NWAC Observations that facets between crust layers in the mid pack gave a Q1 shear but did not show a tendency to propagate via an ECT. The Mission Ridge ski patrol Sunday reported a surface rain crust with no natural or ski cut avalanches.

Some sun with mild temperatures is being seen east of the crest on Wednesday. Small loose wet avalanches might be possible on steep solar slopes.

The south-east Cascades away from the crest will likely have a lower avalanche danger.   

The overall snowpack remains well below normal for this time of year and some windward or southerly aspects have little if any snow cover.

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.

Elevations: Alpine, Treeline.

Likelihood

Possible

Expected Size

1 - 1

Valid until: Jan 22nd, 2015 10:00AM