Avalanche Forecast

Issued: Nov 30th, 2016 10:09AM

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

Recent wind slabs may linger Thursday, but slowly stabilize. Also, watch for  local cornices along ridges. Be prepared to alter plans if local snow and avalanche conditions warrant.

Summary

Detailed Forecast

Another break between systems is expected Thursday as brief high pressure transits the region. There may be a few showers early Thursday to midday, but little accumulation is expected. Winds should be light Thursday.

This should allow for recent storm snow and any wind slabs below ridges to begin settling.  The greatest concern Thursday should be on steep lee slopes below ridges that may have wind transported snow deposited Wednesday. These slopes should range from NW-E facing. 

In addition, watch for any recent cornice formations along ridges and give these early season cornices a wide birth as they may be fragile.   

In much of the lower elevation, below treeline band, there is insufficient snow to produce avalanches, but watch for early season hazards such as rocks and creeks.  Avalanche problems should be limited to the upper part of this elevation band and higher elevations.

Snowpack Discussion

Weather Discussion for the Cascade West Slopes

After a stormy Thanksgiving weekend, which especially hammered the Mt. Baker area, a frontal passage Sunday night was followed by a period of NW flow that dropped 4-12 inches of snow along the west slopes of the Cascades through Monday morning. A few additional inches accumulated during the day Monday with light to moderate showers and snow levels around 3500-4000 feet. Tuesday was a break between weather systems.

The most recent storm began about midnight Wednesday, Nov. 30 with new snow ranging from 8-14 inches as of late Wednesday afternoon at most west slope NWAC stations. Ridgetop winds initially were moderate southerly, shifting to more westerly and diminishing greatly by Wednesday afternoon.  

Recent Reports for the Cascade West Slopes

Monday, Alpental pro-patrol found a homogeneous 2 ft of recent storm snow on top of older snow at the top of their hill with an average snowdepth of 3 ft (1 m) above 5000 ft although snowdepths varied widely depending on wind effect. Low quality shears were found in snowpack tests and there were no layers of concern within the new storm snow.  

DOT professionals were on Chinook Pass Monday and found a well bonded snowpack with generally dense surface snow.  

Wednesday, NWAC pro observer Dallas Glass in the backcountry of Crystal Mountain found a right side up snowpack with 4-6 inches of storm snow well bonded to the older settled snow. No avalanches were seen and no evidence of wind effects or layers of concern was noted.   

Also Wednesday, Mt. Baker pro-patrol reported only minimal recent storm snow avalanches from control work. These avalanches ranged up to about 5 inches and all within the most recent storm snow since midnight. No significant storm layer or older layers were noted. 

In general, much of the below tree-line elevation band still has plenty of terrain anchors, but these are filling in quickly with each passing storm.  The near and above treeline bands have been filling in throughout the west slopes of the Cascades, but are the most shallow in the Pass zones including Stevens, Snoqualmie and White. 

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

Possible

Expected Size

1 - 1

Valid until: Dec 1st, 2016 10:09AM