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Turnagain Pass Avalanche Forecast RSS

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ARCHIVED FORECAST - All forecasts expire after 24 hours from the posting date/time.
Issued
Sun, February 15th, 2015 - 7:00AM
Expires
Mon, February 16th, 2015 - 7:00AM
Forecaster
Wendy Wagner
The Bottom Line

The avalanche danger remains CONSIDERABLE in the Alpine elevations (>2,500′) for triggering a slab avalanche 10-20″ thick. These slabs are sitting on very weak faceted snow and a high likelihood exists for triggering one on slopes steeper than 35 degrees. Below 2,500′ in the Treeline elevation band, there is a MODERATE danger where wet loose and possibly wet slab avalanches can be triggered on steep slopes and gully sidewalls.

*The avalanche danger is expected to rise tomorrow as a very warm and wet storm is on the doorstep.

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Sun, February 15th, 2015
Alpine
Above 2,500'
Considerable (3)
Avalanche risk
Treeline
1,000'-2,500'
Moderate (2)
Avalanche risk
Below Treeline
Below 1,000'
No Rating (0)
Avalanche risk
Alpine
Above 2,500'
Avalanche risk
Considerable (3)
Treeline
1,000'-2,500'
Avalanche risk
Moderate (2)
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

Strong Easterly winds yesterday, along with a powerful warm storm moving in this evening, will keep our tenuous snowpack on the brink. Although visibility was limited yesterday, we were able to see two natural slab avalanches (~12″ thick with wide propagation) that occurred sometime early in the morning. These were on the North side of the Magnum Ridge on Turnagain Pass where winds commonly cross-load the North facing gully features (photo below). With a well-documented layer of weak faceted snow underlying the recent snowfall from February 11th, it is not a surprise to see this natural activity. 

Although there are variations in snowpack structure region-wide (Girdwood Valley to Turnagain Pass to Summit Lake), the set-up for today and coming into this evening’s storm is similar: Essentially, we have very weak faceted snow that sits under dense slabs anywhere from 4-20″ thick. Some of these slabs are older and some newer, but nonetheless we have weak snow under them. Along with that, below 3,500′ many of these slab-weak layer combos have a slick melt-freeze crust underneath; this can act as a bed surface and encourage propagation of a slab if one is triggered

Before the addition of snow and wind later tonight for nature to start tipping the balance, human triggered avalanches will be likely. These areas are mainly confined to upper elevation steep slopes over 35 degrees harboring a slab 6″ thick or thicker. Watch for collapsing and cracking and triggering an avalanche remotely will be possible. With a bit less-than-desirable surface conditions below 3,000′, it may be best to let this next storm roll through before venturing down to Turnagain Pass.

 

 

Avalanche Problem 2
  • Wet Loose
    Wet Loose
Wet Loose
Wet Loose avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.
More info at Avalanche.org

Warming temperatures and rain on snow up to 2,000′ later tonight will keep wet avalanche activity on the radar. Although a superficial re-freeze has likely occurred overnight and we only saw a few wet loose avalanches yesterday, a higher rain/snow line should re-activate and encourage wet slides. With a poor snowpack structure in the top 1-2′ of the snowpack, the potential is there to see shallow wet slab avalanches along with the typical wet loose variety.

Weather
Sun, February 15th, 2015

Yesterday’s weather boiled down to overcast skies, strong Easterly winds and little precipitation. See the tables below for exact numbers. Although little precipitation was seen on the Pass itself, it was raining moderately on the far Northern end and in Portage Valley. The rain/snow line was around 1,500′ and seemed to lower slightly through the day.

This morning we should see a brief lull between storms as winds and showery precipitation have died down. The Satellite image (seen below from 6am) is showing a large – and warm – plume of moisture headed our way later today. Expect winds to pick up to the 30’s mph from the East this afternoon, visibility to shut down and light rain begin to fall up to 2,000′. Temperatures should remain in the upper 30’s F at 1,000′ and warm to ~30F on ridgetops.

 

Beginning this evening and into tomorrow, gale force winds, rain up to 2,500′ (or higher) and around 2″ or more of water amounts are expected!! The good news with this system is that the models are showing colder air wrapping in for Monday evening; this will hopefully lower the rain/snow line before it stops precipitating. Stay tuned on tomorrow’s advisory.

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

  Temp Avg (F) Snow (in) Water (in) Snow Depth (in)
Center Ridge (1880′) 36   rain   0.1   35  
Summit Lake (1400′) 35   0   0   9  
Alyeska Mid (1700′) 35   rain   0.24   25  

RIDGETOP 24-hour data (6am – 6am)

  Temp Avg (F) Wind Dir Wind Avg (mph) Wind Gust (mph)
Sunburst (3812′) 27   E   25   58  
Seattle Ridge (2400′) 29   NE   20   40  
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Riding Areas
Updated Fri, May 01st, 2020

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
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Closed
Skookum Drainage
Closed
Turnagain Pass
Closed
Closed as of May 1. Thanks for a fun, safe season!
Twentymile
Closed
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Carter Lake
Closed
Lost Lake Trail
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Snug Harbor
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Closed

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This is a general backcountry avalanche advisory issued for Turnagain Arm with Turnagain Pass as the core advisory area. This advisory does not apply to highways, railroads or operating ski areas.