Turnagain Pass Avalanche Forecast RSS

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ARCHIVED FORECAST - All forecasts expire after 24 hours from the posting date/time.
Issued
Tue, April 7th, 2015 - 7:00AM
Expires
Wed, April 8th, 2015 - 7:00AM
Forecaster
Wendy Wagner
Avalanche risk The Bottom Line

There is a  CONSIDERABLE avalanche danger in the Girdwood Valley and other favored areas that receive 8-16+” of new snow by this afternoon. New snow combined with strong Easterly winds will create a variety of storm snow instabilities.  These include wind slabs (up to 2′ thick), loose snow avalanches and cornice falls. Natural avalanches are possible and human triggered avalanches are likely. Careful snowpack evaluation and conservative route-finding is essential in avalanche terrain.

*Today’s avalanche danger will depend on the amount of new snow that accumulates. Some areas, possibly Turnagain Pass itself, will only see around 6″ of new snow and will have a MODERATE danger – in this case.

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Tue, April 7th, 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
  • Storm Slabs
    Storm Slabs
Storm Slabs
Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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

A quick moving storm is impacting most areas in Southcentral Alaska this morning. Anywhere from 6-16″ of new snow is possible depending on what areas in the Girdwood/Portage/Turnagain Pass regions are favored. Gale force Easterly winds on the other hand are equally impacting the ridgetops across the regions; Sunburst weather station is averaging in the 60’s mph with gusts in the 90’s. Precipitation began last night and as of 6am this morning, storm totals are:

Girdwood Valley –  1.1″ of water at Alyeska’s Top station (2800′) = ~10+” of snow 
Turnagain Pass –  0.2″ of water (1880′) = 3-4″ of snow in the Alpine
Summit Lake –  0″ 

Another 5-7″ of snow is expected today on top of the totals above at the higher elevations. Along with a storm day comes your garden variety storm snow issues, listed below. These issues are dependent upon the amount of new snow that falls. Turnagain Pass seems to be on the losing end so far but may see a bump in precip later this morning. Bonding with the old snow surface is expected to be initially poor, especially on South, West and East aspects due to a slick and hard pre-existing sun crust.

WIND and STORM SLABS:
With such strong winds, most slabs formed today will have a wind component, even in the lower elevations. Wind slabs could build as thick as 2+’ in higher snowfall zones but will likely be around 8-12″ in the Turnagain Pass area. Watching for current wind loading and cracking in the snow around you, as well as performing quick hand pits and using a pole to feel for stiff snow over softer snow, are all good ways to suss out slabs.

LOOSE SNOW AVALANCHES:
Sluffs should be expected in areas out of the wind. These are likely to run fast and far on aspects with a crust underneath. Additionally, damp or wet snow sluffs, within the new snow, will trigger easily with the first warming by the sun (possibly late today or tomorrow).

CORNICES:
Cornices will increase in size with this storm and may fail naturally triggering an avalanche below – similar to last week.

Avalanche Problem 2
  • 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

North facing aspects above 2,000′ have a variety of weak faceted layers 2-3′ below the surface. For the most part these have adjusted to the current load, however with additional load today (new snow and wind) they have the potential to re-activate. This means either a storm snow avalanche could ‘step-down’ and trigger and deeper slide lower on the slope, or a slab could fail initially in these old weak layers. Either way, Northerlies harbor potential for large slab avalanches.

If you find yourself hunting for fresh snow after this storm, be aware that a slab avalanche breaking in old snow 2-3+’ down is possible on steep North facing terrain. 

Weather
Tue, April 7th, 2015

Overcast skies and windy conditions filled the region yesterday as a large low-pressure system in the Bering pushed a moist frontal band our way. Ridgetop winds ramped up later in the day with averages around 30mph from the East. Temperatures were in the mid 20’s F on the ridgetops and near 40F at 1,000′.  Overnight, precipitation began falling with rain below 1,500′ and as of 6am this morning we have seen around 10″ of snow in the upper elevations in Girdwood Valley yet only 3-4″ at Turnagain Pass.  

Today, we should see another .5-.7″ of rain below 1,500′ and 5-7″ of snow above. The bulk of the precipitation should end by mid-day with a chance for skies to break later this afternoon. Ridgetop winds will remain in the gale force category with averages between 40-65mph and gusts up to 90mph from the East; winds should die off late in the day. Temperatures look to increase to the upper 20’s F on the ridgetops before cooling off quickly with the end of the precipitation.

Check out this radar link for a good look at the frontal passage and trailing dry line (end of main precip event).

Radar image below is from 6:57am this morning:

Wednesday looks to be mostly cloudy with light showers before another similar quick moving front moves through on Thursday.

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

  Temp Avg (F) Snow (in) Water (in) Snow Depth (in)
Center Ridge (1880′) 33   2   0.2   59  
Summit Lake (1400′) 37   0    0 9  
Alyeska Mid (1700′) 33   1   0.67   35  

RIDGETOP 24-hour data (6am – 6am)

  Temp Avg (F) Wind Dir Wind Avg (mph) Wind Gust (mph)
Sunburst (3812′) 25   ENE   34   94  
Seattle Ridge (2400′) 27   n/a   30 66  
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Riding Areas
Updated Thu, April 01st, 2021

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
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Open
No parking in turnaround at end of the road near the outhouse.
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Open
Please do not ride along Railroad tracks. Cross tracks at 90 degree angle and clear the right of way.
Skookum Drainage
Closed
The Skookum Valley is closed to snowmachines. This closure occurs annually on April 1 as per the CNF Forest Plan.
Turnagain Pass
Open
Twentymile
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Please do not ride along Railroad tracks. Cross tracks at 90 degree angle and clear the right of way.
Seward District
Carter Lake
Open
Lost Lake Trail
Open
Primrose Trail
Open
Resurrection Pass Trail
Closed
Closed for the 2020/21 winter season.
Snug Harbor
Open
South Fork Snow River Corridor
Open
Summit Lake
Open

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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.