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ARCHIVED FORECAST - All forecasts expire after 24 hours from the posting date/time.
Issued
Thu, December 8th, 2016 - 7:00AM
Expires
Fri, December 9th, 2016 - 7:00AM
Forecaster
Heather Thamm
The Bottom Line

A MODERATE avalanche danger exists on all aspects above 2000′ where triggering an avalanche 1-2+’ thick is possible on slopes steeper than 35 degrees. Triggering an isolated wind slab avalanche is also possible today near ridgetops that have been loaded by winds over the past week.  Below 2000′ in the trees where the snow is loose and unconsolidated the avalanche danger remains  LOW.

If headed to Summit Lake check out the Summit Lake Summary  HERE.

***Out of area:  Click HERE to check out an observation about a human triggered avalanche in the Anchorage Front Range on Dec. 5.

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Thu, December 8th, 2016
Alpine
Above 2,500'
Moderate (2)
Avalanche risk
Treeline
1,000'-2,500'
Low (1)
Avalanche risk
Below Treeline
Below 1,000'
No Rating (0)
Avalanche risk
Alpine
Above 2,500'
Avalanche risk
Moderate (2)
Treeline
1,000'-2,500'
Avalanche risk
Low (1)
Below Treeline
Below 1,000'
Avalanche risk
No Rating (0)
Danger Scale:
No Rating (0)
Low (1)
Moderate (2)
Considerable (3)
High (4)
Extreme (5)
Avalanche Problem 1
  • Persistent Slabs
    Persistent Slabs
Persistent Slabs
Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.
More info at Avalanche.org

A 1-2+’ slab sitting on top of a widespread layer of buried surface hoar continues to warrant caution in the alpine throughout Turnagain Pass. This layer was formed in mid November and was the cause of  dozens of human triggered avalanches over several weeks. Observers continue to find this layer on all aspects above 2000’ and many stability tests still show propagation potential.  However without any major weather factors adding stress to the snowpack this layer is becoming more stubborn and difficult to trigger with time. The places most suspect are large steep slopes (>35 degrees) that haven’t avalanched. Since we don’t have X-ray vision of the entire snowpack and evidence of natural avalanche activity was limited during several storms, uncertainty exists in terrain that hasn’t seen much traffic. The presence of surface hoar within the snowpack should be part of your slope choices today especially if you are venturing into steeper untracked areas. Consider the consequences of an avalanche before committing to a route and always use safe travel protocols. 

  • Expose one person at a time
  • Group up in safe zones
  • Have an escape route planned
  • Watch your partners and be aware of other groups around you

 The two photos below are examples of where the buried surface hoar continues to be reactive in test pits. Check out observations from Dec.6 at Sunburst and Dec.5 at Tincan.  

Avalanche Problem 2
  • Wind Slabs
    Wind Slabs
Wind Slabs
Wind Slab avalanches are the 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.
More info at Avalanche.org

Several wind events over the last week have formed wind slabs near and below ridgetops on a variety of aspects.  Stiff supportable wind slabs formed in thin rocky areas may pop once you are out onto the slab. Be wary of hard over soft snow, hollow sounds and steep slopes with obvious deposition in the start zone.

Weather
Thu, December 8th, 2016

Yesterday was overcast with low temperatures around 15F and highs around 23F. Winds were calm. No new precipitation was recorded in Turnagain Pass, and an inch of snow fell in Girdwood overnight.  

Today skies will be mostly sunny with a chance of light snow showers. Expect light ridgetop winds to be shifting from the East to a more Northerly direction and temperatures will be in the teens (F) to low 20F’s.  

A similar pattern is expected into the weekend with temperatures dipping back into the single digits and possibly cooler.

PRECIPITATION 24-hour data (6am – 6am)

  Temp Avg (F) Snow (in) Water (in) Snow Depth (in)
Center Ridge (1880′) 21   0   0   19  
Summit Lake (1400′) 16   0   0   4  
Alyeska Mid (1700′)  18 .05   1   8  

RIDGETOP 24-hour data (6am – 6am)

  Temp Avg (F) Wind Dir Wind Avg (mph) Wind Gust (mph)
Sunburst (3812′) 20   ENE   4   17  
Seattle Ridge (2400′) 23    ESE 1   2  
Observations
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Riding Areas
Updated Wed, December 11th, 2019

Status of riding areas across the Chugach NF is managed by the Glacier and Seward Ranger Districts, not avalanche center staff. Riding area information is posted as a public service to our users and updated based on snow depth and snow density to prevent resource damage at trailhead locations. Riding area questions contact: mailroom_r10_chugach@fs.fed.us

Area Status Weather & Riding Conditions
Glacier District
Johnson Pass
Closed
Closed.
Placer River
Closed
Closed.
Skookum Drainage
Closed
Closed.
Turnagain Pass
Closed
Closed.
Twentymile
Closed
Closed.
Seward District
Carter Lake
Closed
Closed.
Lost Lake Trail
Closed
Closed.
Primrose Trail
Closed
Closed.
Resurrection Pass Trail
Closed
Closed. Will be open for the 2019/20 season pending adequate snow cover.
Snug Harbor
Closed
Closed.
South Fork Snow River Corridor
Closed
Closed.
Summit Lake
Closed
Closed.

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