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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, January 6th, 2013 - 7:00AM
Expires
Mon, January 7th, 2013 - 7:00AM
Forecaster
Wendy Wagner
The Bottom Line

We continue to have dangerous avalanche conditions in the backcountry. The failure of weak snow near the base of the snowpack has resulted in large and destructive avalanches during the past week. Additionally, a few inches of new snow today with strong wind will create smaller but sensitive wind slabs on the surface. These two types of avalanche problems will keep the danger pegged at CONSIDERABLE. Human triggered avalanches are likely near and above treeline on slopes 35 degrees and steeper. Below treeline the danger is MODERATE where triggering a slide is possible. Expert level route finding and terrain management is required for a safe day in the mountains.

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Sun, January 6th, 2013
Alpine
Above 2,500'
Considerable (3)
Avalanche risk
Treeline
1,000'-2,500'
Moderate (2)
Avalanche risk
Below Treeline
Below 1,000'
Moderate (2)
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
Moderate (2)
Danger Scale:
No Rating (0)
Low (1)
Moderate (2)
Considerable (3)
High (4)
Extreme (5)
Avalanche Problem 1
  • Deep Persistent Slabs
    Deep Persistent Slabs
Deep Persistent Slabs
Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.
More info at Avalanche.org

Once again our primary concern will be deep slab avalanches. This is simply due to the size and destructive power this type of avalanche can produce. As the weak faceted snow from October and November is getting deeper and deeper in the pack (4-10′) it is easy to focus on what is going on at the surface – today that will be wind slabs. But we can’t forget that lurking below, where obvious signs of instability are minimal to none, there is a weak layer of snow that is struggling to hold the entire snowpack to the slopes. Triggering a deep slab is not something to get mixed up in and can have deadly consequences. The best practice is to use safe travel techniques and stick to lower angle terrain.

The cloudy skies and low visibility yesterday hampered a good look around the mountains and with no reported slides from others, there are no new avalanches to pass on. The most recent activity we know of is from 48 hours ago on Jan. 4th  where two large slides released naturally. The most significant for the Turnagain Pass folk is the class 3 slide on Seattle Ridge. These events should not be forgotten as the weak layer responsible is over a month old and slab is 2 weeks old, hence the persistence issue.

Remember, the only obvious clue as to a deep slab problem is the knowledge weak snow exists near the ground. All other signs of instability such as cracking and collapsing, including recent avalanches, is not a sign the problem has gone away. A guilty until proven innocent situation.

If you’re interested in a little deep slab reading, here is a good article from our friends in Colorado.

Avalanche Problem 2
  • Wind Slabs
    Wind Slabs
Wind Slabs
Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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

Yesterday we found a few small pockets with shallow wind slabs (4-8” thick) at treeline. These were quite reactive to a person as they were in the formation stage and fresh. This should be the case again today with a few more inches of snow and wind that will load leeward slopes. Above treeline slabs will be larger (in the 1 foot or more range) and with the underlying weaknesses at the bottom of the pack, it would not be unexpected for a smaller wind slab to step down and trigger a much larger deep slab.

Weather
Sun, January 6th, 2013

The progressive weather pattern we have been in for the past 2 weeks, that has brought us cloudy skies, snow and wind, continues. Yesterday we picked up around 3 € of snow at mid elevations with rain below 800′. Winds blew in the 30’s with gusts to 50mph from the east. Remember we have weather history charts for those interested.

Today should be similar with an additional 2-4 € of snow and rain up to 6-800′. Winds will remain strong out of the east averaging ~30mph with gusts to 50mph on the ridgetops. Temperatures are currently in the mid 20’s above treeline and mid 30’s below and should cool a degree or two through the day.

A larger system moves in this evening that looks to bring around a foot of new snow tonight into Monday with slightly cooler temperatures. A break in the weather Tuesday into Wednesday may bring a welcome shot of sunshine.


John will issue the next advisory on Monday, January 7th.

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Riding Areas
Updated Mon, October 26th, 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
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

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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.