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Archived

Avalanche Forecast

Apr 2nd, 2014–Apr 3rd, 2014
Alpine
2: Moderate
The avalanche danger rating in the alpine will be moderate
Treeline
2: Moderate
The avalanche danger rating at treeline will be moderate
Below Treeline
1: Low
The avalanche danger rating below treeline will be low
Alpine
3: Considerable
The avalanche danger rating in the alpine will be considerable
Treeline
2: Moderate
The avalanche danger rating at treeline will be moderate
Below Treeline
2: Moderate
The avalanche danger rating below treeline will be moderate

Regions: Snoqualmie Pass.

Watch for older but still sensitive wind slab on a variety of aspects, not just the traditional lee NW thru SE aspects near and above treeline indicated on the elevation/aspect diagram. 

Detailed Forecast

Increasing cloud cover and ridgetop winds paired with relatively cool snow levels should help minimize wet loose concerns Thursday.  New loading is not expected to be significant during the daylight hours Thursday. 

However, wind slab may locally still be sensitive on a variety of aspects near and above treeline, especially in the south and central Washington Cascades were recent east winds loaded and cross loaded unusual aspects.  Watch for signs of cracking or firmer wind transported snow and approach open lee slopes with caution.

Remember to watch for cornices if you venture onto ridges and avoid slopes below cornices. Cornice failures are often seen during the transition to spring weather. Cornices have grown large recently and often break back much further than anticipated. 

Snowpack Discussion

March ended with a return to winter; a storm cycle that began last week peaked over the weekend and delivered about 1 to 3.5 ft of snow at NWAC stations near and west of the crest, with the highest totals near Mt. Baker and higher elevation sites. Natural avalanche cycles were seen over weekend with several skier/rider triggered slabs; more on these below.  An upper low that spun into California largely missed the PNW early this week, but easterly winds in the near and above treeline zones late Sunday night through early Tuesday have cross loaded slopes mainly over the south Cascades, but perhaps as far north as the central Cascades. Since Monday, afternoon temperatures have been climbing well above freezing and storm weaknesses from the weekend should have quickly settled and stabilized.  

Recent avalanche observations:  Increasing rain and snow, winds and warming temps began the increase in avalanche activity Friday with sensitive storm slab in the afternoon. On Saturday at Mt. Baker wet loose releases were reported below 4000 ft with building winds slab near and above treeline. Over the weekend, (likely Sat) TAY reports indicated that there were human triggered slabs up to 1' along the upper Shuskan Arm traverse and in the Blueberry Chutes area that may have resulted in a partial burial. Skier triggered storm slabs on lee slopes were reported in Silver Basin near Crystal on Saturday on the NWAC observation page. Sunday the Mt Baker and Alpental ski patrols reported isolated 4-8 inch storm slab avalanches releasing in storm layers. Also on Sunday, a TAY post told of several sensitive storm slabs up to 1' found on lee northerly aspects in Castle Bowl in the Tatoosh range. One skier triggered slab took a skier for a ride, but luckily no injuries were reported.   

 

Multiple snowmobile triggered shallow storm slabs on W-NW aspects near tree line were observed on Grouse Mountain near Mt Baker Sunday, 3/30 by NWAC observer Jeff Hambelton.  Photo: J. Hambelton 

NWAC observer Dallas Glass on Mt. Rainier Tuesday reported that the moderate east winds from earlier in the week had redistributed and cross loaded a variety of aspects above treeline, forming 20-40 cm of wind slab with a few natural avalanches.  Dallas also reported that with clearing Tuesday afternoon, small wet loose slides released on solar aspects. On Wednesday, Jeff Hambelton in the Mt. Baker area reported relatively cold snow still found on sheltered non-solar aspects and cornices that had grown larger the most recent storm cycle.  A few had released in last day or two, but generally only entrained shallow amounts of wet surface snow.

Avalanche Problems

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