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Archived

Avalanche Forecast

Jan 10th, 2014–Jan 11th, 2014
Alpine
4: High
The avalanche danger rating in the alpine will be high
Treeline
3: Considerable
The avalanche danger rating at treeline will be considerable
Below Treeline
2: Moderate
The avalanche danger rating below treeline will be moderate
Alpine
4: High
The avalanche danger rating in the alpine will be high
Treeline
4: High
The avalanche danger rating at treeline will be high
Below Treeline
3: Considerable
The avalanche danger rating below treeline will be considerable

Regions: Olympics.

An active, complex weather pattern will cause rapidly changing snow and avalanche conditions Friday and Saturday so paying attention to weather and snow conditions and being willing to change plans will be especially important.

Detailed Forecast

The forecast for Friday is a more complex than usual.

An occluded front should cross the Northwest Thursday afternoon and evening. This should cause continued west to southwest winds and a few more inches of snow Friday morning. This should maintain similar conditions through Friday afternoon. Watch for wind slab on lee slopes mainly north to southeast aspects. Storm slab may be possible on more varied aspects. Less snow and lighter winds as well as continued low snow depths should cause less avalanche danger at lower elevations.

The complex part of the forecast comes Friday afternoon and evening which will be a period of rapid change. A very strong front is indicated to cross the Northwest on Friday night. Currently it looks like the strongest winds, heaviest rain or snow and main warming will hold off through Friday afternoon and then begin Friday evening. The avalanche danger should greatly increase Friday night. Beware that if this system and these changes arrive sooner the avalanche danger could rapidly increase Friday afternoon.

Snowpack Discussion

The last storm cycle was late last week. The most significant avalanches from that period were human triggered 1-1.5 foot wind or storm slab avalanches reported Saturday from Mt Herman near Mt Baker and from Chair Peak near Alpental.

Sunny weather with increasingly warm temperatures were seen Sunday and Monday which produced some small loose wet slides on solar aspects and crusts on more varied but not all aspects. Less warming was seen in the passes due to cooler easterly flow. 

Weak systems began to move to the Northwest about Tuesday with persisting cool offshore surface flow. This caused light rain or snow and a mix of precipitation in the passes.

A stronger system moved across the Northwest on Wednesday. Snowfall at NWAC sites near and west of the crest was in the 6-17 inch range with the most at Mt Baker. An overall cooling trend Tuesday and Wednesday helped to bond new snow to older or crusted surfaces from Sunday and Monday and built mostly favorable new snow profiles.

The most relevant available reports on Thursday are from the ski areas. In summary isolated or local small storm or wind slabs up to a about a foot were reported from Mt Baker, Stevens and Alpental on Thursday with the releases within the new snow and with generally favorable new snow profiles. Isolated shallow storm slab of only a couple inches was generally seen at Crystal. Reports confirmed that bonds were generally good to older or crusted surfaces from Sunday and Monday.

Mostly light snow showers with minor temperature changes on Thursday should be generally maintaining these conditions.

Reports also seem to indicate that hoar frost seen early in this week generally didn't survive the changes or is not reactive. Reports indicate generally stable crusts and melt forms in the mid and base pack in this area.

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.

Elevations: Alpine, Treeline.

Likelihood: Likely

Expected Size: 1 - 1