Support the forecast! Support the forecast!

Give to Friends of the Chugach National Forest Avalanche Info Center.

Turnagain Pass Avalanche Forecast RSS

Archives
ARCHIVED FORECAST - All forecasts expire after 24 hours from the posting date/time.
Issued
Sun, February 4th, 2018 - 7:00AM
Expires
Mon, February 5th, 2018 - 7:00AM
Forecaster
Wendy Wagner
The Bottom Line

A generally  LOW  avalanche danger exists in the mountains surrounding Turnagain Pass. Although triggering an avalanche large enough to bury a person is unlikely, isolated slabs 1-2′ deep can still be found in steep and/or wind loaded areas.  LOW danger does not mean No Danger.  Evaluate the consequences of terrain before committing to a slope. Additionally, watch for cornices along ridgelines and sluffs in steep terrain.  

*In the periphery zones of Girdwood to Portage Valley, and Johnson Pass to Summit Lake more caution is advised where a slab could be larger and more connected.

Check out the Summit Lake Summary  HERE.  

Thanks to our sponsors!
Sun, February 4th, 2018
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
  • Persistent Slabs
    Persistent Slabs
  • Almost Certain
    Very Likely
    Likely
    Possible
    Unlikely
    Likelihood
  • Historic
    Very Large
    Large
    Small
    Size
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.

Likelihood of Avalanches
Terms such as "unlikely", "likely", and "certain" are used to define the scale, with the chance of triggering or observing avalanches increasing as we move up the scale. For our purposes, "Unlikely" means that few avalanches could be triggered in avalanche terrain and natural avalanches are not expected. "Certain" means that humans will be able to trigger avalanches on many slopes, and natural avalanches are expected.

Size of Avalanches
Avalanche size is defined by the largest potential avalanche, or expected range of sizes related to the problem in question. Assigned size is a qualitative estimate based on the destructive classification system and requires specialists to estimate the harm avalanches may cause to hypothetical objects located in the avalanche track (AAA 2016, CAA 2014). Under this schema, "Small" avalanches are not large enough to bury humans and are relatively harmless unless they carry people over cliffs or through trees or rocks. Moving up the scale, avalanches become "Large" enough to bury, injure, or kill people. "Very Large" avalanches may bury or destroy vehicles or houses, and "Historic" avalanches are massive events capable of altering the landscape.

Signal Word Size (D scale) Simple Descriptor
Small 1 Unlikely to bury a person
Large 2 Can bury a person
Very Large 3 Can destroy a house
Historic 4 & 5 Can destroy part or all of a village
More info at Avalanche.org

Another brilliant sunny day is on tap and with that, another day for folks to travel well into the mountains. This is the 10th day of cold and clear weather, which has been steadily increasing the stability of the snowpack. Tracks litter most slopes around Turnagain Pass, and though we have moved into a LOW danger regime, there still remains isolated areas where a person can trigger a slab avalanche. We saw this yesterday in the Twin Peaks area where a foot deep slab was triggered by a party on the uptrack. There were already many tracks on the slope when it released and skiers were ascending the same track they used earlier that day. There was one person caught on the slab who was able to get off it quickly and luckily no one was carried down. This area is on the Southern edge of the forecast zone, in the periphery, where a shallower snowpack exists. 

If you are headed out today, keep the following avalanche problems in mind:

Persistent Slabs:  A layer of buried surface hoar exists roughly 1-2′ deep and has been responsible for the scattered avalanche activity over the past 10 days. Last night a report came in from Eddies SW face where two people were caught and carried in a slab last Friday (all are ok). Again several tracks were on the slope before a person found just the wrong spot that presumably had prior wind loading. Amongst all the soft snow out there, watch for these pockets where winds have stiffened and/or loaded areas. These are the most likely places to find an isolated slab. Although most of these slabs have been relatively small, larger slabs could be lurking as was found in the Twin Peaks zone. If choosing to push into the steep and committing terrain, identify terrain traps like gullies, cliffs or rocks below to consider the consequences if even a small slab is released. Again, in the periphery areas of Girdwood, Placer Valley, Johnson Pass and Summit Lake more caution is advised due to higher winds last week and the potential for larger slabs to be found.  

 *Deep Persistent Slab:  Weak snow can still be found near the ground at the upper most elevations in our forecast area, 3,000′ – 5,000′. Although triggering a Deep Persistent Slab is very unlikely, it is worth keeping in mind that poor structure does exist at the high elevations. 

Loose Snow ‘sluffs’:  In most places the snow is too loose to form a slab and the surface snow ’sluffs’ easily on the steeper slopes. Expect loose dry snow to be fast moving in steep terrain and don’t be surprised if it knocks you over as it picks up speed. Manage your ‘sluff’ and be aware of the consequences below you.

Cornices:  Cornices are unpredictable and can break further back along a ridge than expected. Give these features plenty of space. 
 

Pictured below is the avalanche triggered on Twin Peaks Saturday, Feb 3rd. This slab is thin, ~ a foot thick, but shows wide propagation across the slope (photo: Andy DuComb). 

 

View of skin track with crown of the slab on Twin Peaks (photo: Mark Norquist)

Weather
Sun, February 4th, 2018

Another cold and clear sky day was had yesterday in the mountains. While single digits temperatures remained in place in valley bottoms, ridgetops climbed into the teens F. Ridgetop winds were Easterly and generally light, 5-10mph with a few gusts reaching 20mph. An impressive inversion is yet again in place this morning with Johnson Pass trailhead at -16F while ridgetops (Sunburst and Seattle Ridge) are close to 20F.  

Today will see sunny skies once again, yet warmer air is slowly sliding in from the East. Ridgetops have bumped to near 20F as of this morning and could increase to the mid-20’s today. Ridgetop winds are forecast to be light and variable, shifting Easterly in the 5-10mph range tonight. Valley bottoms are likely to remain generally chilly through the day.  

For tomorrow, Monday, the blocking high-pressure over Alaska will begin to push North and allow a moist low-pressure system to move into Southcentral. Clouds and warmer temperatures are expected to stream in Monday. Early Tuesday morning this system “will be delivering a fresh batch  of snow to the Kenai Peninsula and Prince William Sound” according to the National Weather Service. Stay tuned!

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

  Temp Avg (F) Snow (in) Water (in) Snow Depth (in)
Center Ridge (1880′) 19   0   0   62  
Summit Lake (1400′) 9   0   0   18  
Alyeska Mid (1700′) 18   0   0   50  

RIDGETOP 24-hour data (6am – 6am)

  Temp Avg (F) Wind Dir Wind Avg (mph) Wind Gust (mph)
Sunburst (3812′) 16   NE   8   21  
Seattle Ridge (2400′) 19   SE   6   14  
Observations
Recent Observations for Turnagain Pass
Date Region Location
05/06/20 Turnagain Avalanche: Pastoral Peak, north face
04/10/20 Turnagain Avalanche: Wolverine
04/10/20 Turnagain Observation: Eddies lookers right shoulder
04/09/20 Turnagain Observation: Bench Peak
04/04/20 Turnagain Observation: Tincan
04/04/20 Turnagain Observation: Pete’s North
03/26/20 Turnagain Avalanche: Tincan – Proper (SW facing)
03/26/20 Turnagain Avalanche: Seattle Ridge
03/25/20 Turnagain Avalanche: Sunburst Uptrack @ 2000′
03/24/20 Turnagain Observation: Turnagain – Road Observations
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
Placer River
Closed
Skookum Drainage
Closed
Turnagain Pass
Closed
Closed as of May 1. Thanks for a fun, safe season!
Twentymile
Closed
Seward District
Carter Lake
Closed
Lost Lake Trail
Closed
Primrose Trail
Closed
Resurrection Pass Trail
Closed
Snug Harbor
Closed
South Fork Snow River Corridor
Closed
Summit Lake
Closed

Subscribe to Turnagain Pass
Avalanche Forecast by Email

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.