Turnagain Pass Avalanche Forecast RSS

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ARCHIVED FORECAST - All forecasts expire after 24 hours from the posting date/time.
Issued
Wed, January 9th, 2019 - 7:00AM
Expires
Thu, January 10th, 2019 - 7:00AM
Forecaster
Wendy Wagner
The Bottom Line

A generally  LOW  avalanche danger exists across all elevations bands for the Turnagain area. Triggering a slab avalanche is unlikely but not impossible. Glide cracks may release into avalanches. Limiting/avoiding exposure under them is prudent. Give cornices a wide berth and watch your sluff.

SUMMIT LAKE / JOHNSON PASS / LYNX DRAINAGE:  *** We want to emphasize the difference here! More caution is advised  South of Turnagain Pass.***  Keep in mind buried weak layers exist in the middle and base of the snowpack. More potential for triggering a large slab avalanche exists in this zone. Choose terrain wisely and please read the Additional Concerns below.  

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Wed, January 9th, 2019
Alpine
Above 2,500'
Low (1)
Avalanche risk
Treeline
1,000'-2,500'
Low (1)
Avalanche risk
Below Treeline
Below 1,000'
Low (1)
Avalanche risk
Alpine
Above 2,500'
Avalanche risk
Low (1)
Treeline
1,000'-2,500'
Avalanche risk
Low (1)
Below Treeline
Below 1,000'
Avalanche risk
Low (1)
Danger Scale:
No Rating (0)
Low (1)
Moderate (2)
Considerable (3)
High (4)
Extreme (5)
Avalanche Problem 1
  • Normal Caution
    Normal Caution
Normal Caution
Normal Caution means triggering an avalanche is unlikely but not impossible.
More info at Avalanche.org

LOW danger doesn’t mean NO danger!

Despite our generally stable conditions, it is still important to look for signs of instability as the mountains can surprise us at times. Good travel habits, such as exposing one person at a time, watching your partners and grouping up in safe zones are, as always, key ways to minimize risk. Ease onto steep slopes and be mindful of people below you and on adjacent slopes.

A week of cold/clear weather and lack of wind over our region has allowed the snowpack to stabilize. The last avalanche was triggered a week ago and ongoing snowpack tests point to stable conditions. Hence, we are in the “normal caution” phase of avalanche concerns. These include:

  • Glide avalanches:  
    • Being in the wrong place at the wrong time and getting caught in a glide avalanche remains a concern. Glide cracks are opening and releasing in popular ski and riding terrain throughout the advisory area. It is important to minimize time spent underneath the glide cracks. Glides are completely unpredictable and not human triggered. Be on the lookout for cracks and wrinkled looking snow (often a precursor to cracking). 
  • An outlier slab avalanche: 
    • Triggering a slab avalanche would most likely occur on an exposed ‘unsupported slope’ that sits above a cliff or steep rocky terrain. There may still be pockets of buried surface hoar lurking 2-3′ under the surface in isolated areas.
  • Cornice falls: 
    • Remember cornices often break farther back from ridges than expected. Give them a wide berth.Sluffs on steep slopes: 
  • Sluffs on steep slopes:
    • Sluffs are slowly becoming larger as the cold weather eats away and weakens the surface layers, turning it to sugary facets. 

Look closely, glide cracks and wrinkled snow on Sunburst SW face under the weather station. Photo: Aleph Johnston-Bloom. 

Additional Concern
  • 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

South of Turnagain – Lynx Creek/Johnson Pass/Summit Lake zone:  A poor snowpack structure exists in these areas. The buried surface hoar that we have been talking about over the past week has been found as well as facet/crust combinations in the bottom of the snowpack. The New Year’s storm overloaded a variety of these weak layers as can be seen in photos from the avalanche activity throughout Summit LakeIf you’re headed this way, the snowpack becomes more complex – evaluate terrain exposure and the snowpack as you travel. 

Weather
Wed, January 9th, 2019

Yesterday:   Mostly cloudy  skies, light winds and cold temperatures were over the region. Upper elevation highs were in the low to mid teens, while valley bottom lows were in the single digits.   Ridgetop winds were generally easterly in the 5-10mph with some gusty winds in the mid and lower elevations noted by observers.

Today:    Cold and clear conditions  are expected back today. Very cold air to our north is spilling over the Alaska Range into Southcentral as we speak, increasing ridgetop winds slightly to the 5-15mph range from the NW. Upper elevation temperatures in the teens and single digit temperatures in valley bottoms are  expected to remain today.  

Tomorrow:   Clear skies and cold air will continue to seep down from the north bringing potentially the coldest temperatures for this extended high-pressure Thursday into Friday. When will we thaw out? Possibly this weekend. Kyle Van Peursem, the Avalanche Program lead at the National Weather Service, stated in this morning’s discussionthere is high confidence that the pattern change will  bring much warmer and wetter weather to the region through at  least the middle of next week.

*Seattle Ridge weather station was heavily rimed and the anemometer (wind sensor) was destroyed. We are currently working to replace it.  

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

  Temp Avg (F) Snow (in) Water (in) Snow Depth (in)
Center Ridge (1880′) 16   0   0   55  
Summit Lake (1400′) 6   0   0   20  
Alyeska Mid (1700′)  16 0   0   43  

RIDGETOP 24-hour data (6am – 6am)

  Temp Avg (F) Wind Dir Wind Avg (mph) Wind Gust (mph)
Sunburst (3812′) 12   E   6   15  
Seattle Ridge (2400′) 15  *N/A  *N/A      *N/A
Observations
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Riding Areas
Updated Mon, December 02nd, 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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