Turnagain Pass Avalanche Forecast RSS

Archives
ARCHIVED FORECAST - All forecasts expire after 24 hours from the posting date/time.
Issued
Sat, December 19th, 2015 - 7:00AM
Expires
Sun, December 20th, 2015 - 7:00AM
Forecaster
Wendy Wagner
The Bottom Line

The avalanche danger will be rising to HIGH  today in response to heavy snowfall combined with strong winds in the Turnagain Pass and Girdwood Valley areas. Avalanches occurring naturally are expected at elevations above 1,000′ where new snow and winds are loading the steeper slopes. Human triggered avalanches in these areas are very likely. As the storm continues, traveling in avalanche terrain is not recommended. A MODERATE danger exists below 1,000′ where an avalanche occurring above may run into this zone.

*If you are thinking of heading into the backcountry today, terrain management will be the key in order to stick to mellow slopes and avoid slopes 35 degrees and steeper. This includes runout areas; for instance the bottom of the gullies along the front side of Seattle Ridge.  Once the snowfall stops and skies break up, very careful snowpack evaluation is necessary and a conservative approach is needed before deciding to enter slopes 35 degrees and steeper.  

Thanks to our sponsors!
Sat, December 19th, 2015
Alpine
Above 2,500'
High (4)
Avalanche risk
Treeline
1,000'-2,500'
High (4)
Avalanche risk
Below Treeline
Below 1,000'
Moderate (2)
Avalanche risk
Alpine
Above 2,500'
Avalanche risk
High (4)
Treeline
1,000'-2,500'
Avalanche risk
High (4)
Below Treeline
Below 1,000'
Avalanche risk
Moderate (2)
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 moisture laden storm is currently moving through the Gulf bringing heavy snowfall to elevations above ~800′ and rain below in the Girdwood Valley and Turnagain Pass zones. Winds have been strong with the snowfall from the East – 30-40mph with gusts in the 70’s mph. Snow totals at the mid-elevations from overnight are:

Girdwood Valley:  8-10+”
Turnagain Pass:  9-11+”
Summit Lake:  2-3″

We are expecting an additional 10-15″ to fall today before the storm slows down tonight. A variety of storm snow avalanches are expected today. These include:

WIND SLABS:  With such strong winds associated with the snowfall, much of the avalanche activity is likely to be on wind loaded slopes. These ‘wind slabs’ are expected to be 1-3′ thick and standard storm-induced slabs that are the most unstable during wind loading and directly after, but can stability quickly.
STORM SLABS:  In areas sheltered from the wind we may see slabs release from denser storm snow falling over less-dense snow.
LOOSE SNOW:  Loose snow avalanches are likely on very steep and rocky terrain.

*In addition to the avalanches expected within the storm snow, there is a possibility that a slide could break into weaker layers that reside 2-3′ deep in the pack. If this is the case, then large avalanches could result. More on this below.

Photo: The approach of the storm. This photo was taken yesterday afternoon by Andy Moderow. A soft, but wind affected, pre-existing surface is now covered with 8-10″ of new snow from overnight with another 10″+ today. The good news is, there are no weak layers on yesterday’s surface and bonding with this new load should occur relatively quickly (in a day or so after the storm).

 

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

Around 2-3′ below the snow’s surface sits a layer of weak snow on top of either a hard crust (elevations below 3,000′) or a hard old wind surface (above 3,000′). The weak snow is comprised of facets that are bonding and in some cases surface hoar. In all our pit tests these weak layers are proving to be quite strong and unreactive. However, with a good shock to they system today – around 2″ of water weight rapidly added to the pack – we can’t rule out the potential that these old weak layers may become overloaded and a large avalanche release.

Weather
Sat, December 19th, 2015

We saw a brief break between storms yesterday as skies broke up and snowfall ceased for the middle part of the day. The Easterly winds, on the other hand, remained strong enough that several folks noted plumes on the peaks during the day.  

Overnight, a Pacific storm moved in and has, as of 6am this morning, added up to a foot of new snow at the higher elevations (above the snow stations). See tables below for snowfall and water numbers at the stations. The rain/snow line is hovering right around 800′ currently and expected to remain. Ridgetop winds picked up as well overnight into the 30-40 mph range with gusts in the 70’s. For today, we should see this very stormy weather continue though this evening before the storm starts thinking about moving out.

Tomorrow, we should see instability showers with moderate Easterly ridgetop winds. This means we could see either skies open up a bit or light snow showers. Stay tuned.

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

  Temp Avg (F) Snow (in) Water (in) Snow Depth (in)
Center Ridge (1880′) 29   9   0.7   55  
Summit Lake (1400′) 26   2   0.2   19  
Alyeska Mid (1700′) 31   9   0.66   39  

RIDGETOP 24-hour data (6am – 6am)

  Temp Avg (F) Wind Dir Wind Avg (mph) Wind Gust (mph)
Sunburst (3812′) 23   NE   20   77  
Seattle Ridge (2400′) 25   N/A N/A N/A  
Observations
Recent Observations for Turnagain Pass
Date Region Location
12/06/19 Turnagain Avalanche: Sunburst
12/04/19 Turnagain Observation: Sunburst
12/03/19 Turnagain Observation: Hippy Bowl
12/01/19 Turnagain Observation: Tincan, All elevations
12/01/19 Turnagain Observation: Tincan
11/30/19 Turnagain Observation: Tincan Treeline Plateau/ Common Bowl/ Ridge
11/29/19 Turnagain Observation: Sunburst Ob #2
11/29/19 Turnagain Observation: Sunburst Ob #1
11/27/19 Turnagain Observation: Tincan
11/25/19 Turnagain Observation: Sunnyside
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.

Subscribe to Turnagain Pass
Avalanche Forecast by Email