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Archived

Avalanche Forecast

Feb 7th, 2014–Feb 8th, 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
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

Regions: Olympics.

Watch for isolated and shallow wind slab mainly on non-solar aspects.  Small loose avalanches on steeper slopes are also possible. 

Detailed Forecast

A weather system passing into Oregon Friday night should not produce any appreciable new snow for the Olympics through Saturday morning.  Light snow showers are possible during the day. Temperatures are expected to remain cold with generally light winds.  

Watch for lingering wind slab mainly on non-solar aspects.  Small loose avalanches on steeper slopes are also possible. 

Manage the terrain by avoiding wind loaded lee slopes near and above tree-line. Watch for shooting cracks as a sign of instability. Even a small wind slab in the wrong terrain, i.e. above cliffs or very steep slopes, could have unintended consequences. 

Snowpack Discussion

A storm arrived at the end of January with rising snow levels and rain above 6000 feet for the Olympics before transitioning to snow and colder temperatures. Wind was less of a factor with this event with a more even distribution of storm snow and a general lack of wind slab during the storm cycle. Only about 1-3 inches of additional snow has accumulated in early February. 

Very cold temperatures this week have produced strong temperature gradients in the upper portion of the snowpack. The strong temperature gradient has lead to near surface faceting and a breakdown on recently buried crusts.  Moderate east to southeast winds in the Cascades built new wind slab during the week.  While winds were lighter over the Olympics, low density surface snow was available for transport and may have built shallow new wind slab that is poorly bonded on lee non-solar aspects. No new information has been received about the spatial character of the wind slab or how reactive it might be to human triggering as of 6 pm Friday. 

Regionally the avalanche danger is lower near Hurricane Ridge than in the Washington Cascades where a more diverse snowpack exists. See the Cascades forecast if traveling there.

The mid and lower snowpack west of the crest consists mainly of crusts and melt form crystal layers which have generally not been reactive to to snow pit tests. Low snow amounts are limiting the avalanche danger on many south slopes and at low elevations due to terrain and vegetation anchors.

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, West, North West.

Elevations: Alpine, Treeline.

Likelihood: Possible

Expected Size: 1 - 1