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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, November 18th, 2012 - 7:00AM
Expires
Mon, November 19th, 2012 - 7:00AM
Forecaster
Wendy Wagner
The Bottom Line

Welcome to the new website layout!   We are joining a nationwide trend to give the forest service avalanche centers a similar look and provide information in a consistent manner. The content only has minor changes from last season, but we think you will like the new web interface. Let us know your thoughts.

We are issuing advisories 5 days a week through November on Sat, Sun, Tue, Thur, Fri. The next advisory will be Tuesday November 20th.

BOTTOM LINE
The avalanche danger will remain CONSIDERABLE today above treeline.  The most likely places to trigger an avalanche are upper elevation slopes over 35 degrees on all aspects where a slab overlies the weak snow from October. Very few people have ventured into this upper elevation steeper terrain, but when they do, it seems they don’t have too much trouble triggering an avalanche breaking near the ground. Managing the terrain will be the key to safe backcounty travel. Additionally, watch for fresh wind slabs in exposed areas with the expected 2-4 inches of snow and moderate ridgetop wind. Below treeline, there is a MODERATE avalanche danger.

This bottom line will pertain to monday, November 19th, as well.

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Sun, November 18th, 2012
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
  • 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

With Wednesday’s 6 inches of snow settled to ~4 inches the snow surface was quite inviting yesterday. Several people were out enjoying this on lower angle slopes and tracked up areas such as the front side of Tincan ridge. Reports from yesterday were in the form of whoomphing and collapsing but we did not hear of any avalanche activity. That being said, very few people have ventured past the easier accessed lower angle terrain, or short steeper slopes (several of which have already avalanched).

This “persistent avalanche” problem is guilty until proven innocent. We know the snowpack structure is poor. We know there are, at the very least, scattered slopes hanging in the balance waiting for a trigger. Yet, there is uncertainty as to how widespread these touchy slopes are. With a few more inches of snow possible today, warmer temperatures and increased wind, this will only add to the problem.

We went up yesterday to take a look at the avalanche that was remotely triggered from ~200′ away two days ago, Friday (11/16). This was on a steep slope on the southwest face of Sunburst and proves how unstable the pack is. More details HERE and HERE.

One of the most concerning aspects to our avalanche conditions right now are that the obvious clues so prevalent the past couple weeks are not nearly as obvious anymore – but the avalanche potential remains similar. This means it can be easier to be lured onto a slope before it breaks. The only clue may be the presence of a slab over a weak layer (if one looks for it), but recent avalanches, cracking or collapsing may not be observed. Furthermore, a slope may or may not slide, but if it does, the ride will likely be rocky and unpleasant. These are good things to keep in mind when the ‘go’ – ‘no go’ question comes up.

Below treeline the snowpack is a combination of crusts, low density snow and moist facets. This accompanied with the lack of a slab, mainly due to minimal wind loading, has kept avalanche activity at bay.

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

Fresh wind slabs may be formed today if the expected 2-4″ of snow with 15mph, gusts to 30, ridgetop easterly wind verifies. With the existing loose snow surface there is plenty of snow available for transport if we only see the wind. Any fresh slabs are likely to be shallow but touchy.

Weather
Sun, November 18th, 2012

Mostly cloudy skies with temperatures plummeting into the single digits and low teens greeted backcounty travelers yesterday. A trace of snow fell throughout the day with very light northerly ridgetop winds.

Temperatures have rebounded this morning to ~20F on the ridgetops but are still inverted with mid teens in the lower elevations. Winds have bumped up slightly and are forecast to blow 15mph with gusts to 30mph from the east. Cloudy and obscured skies should keep visibility limited again today and there in a chance for 2-4″ of snow. This unfortunately looks to be our last shot of precip for the next several days to a week. Clear and cold conditions look to set in Monday through Thanksgiving.

____________________________________________________________________________

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).  

Kevin will issue the next advisory Tuesday, November 20th.

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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.