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 8th, 2017 - 7:00AM
Expires
Mon, January 9th, 2017 - 7:00AM
Forecaster
Heather Thamm
The Bottom Line

A  MODERATE  avalanche danger remains in the Alpine where triggering an old wind slab or a deeper hard slab 2+’ thick is possible on steep wind loaded slopes that haven’t avalanched. At Treeline and below there is  LOW  avalanche danger, where triggering an avalanche is unlikely, but not impossible.

In the periphery zones of Girdwood, Johnson Pass and Summit Lake a shallower snowpack exists and it may be easier to trigger a slab avalanche in these areas.  Check out the Summit Lake Summary  HERE.

*** If heading to Hatcher this weekend – unstable conditions exist – check the Hatcher Pass advisory  HERE!    Mark your calendars for the FREE rescue workshop at Hatcher Pass on January 14th. More info  HERE.  

 

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Sun, January 8th, 2017
Alpine
Above 2,500'
Moderate (2)
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
Moderate (2)
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
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

This weekend if choosing to travel in avalanche terrain it is important to remember although the snowpack is wind hardened and tired, it does have a poor structure. There are a variety of weak layers (buried surface hoar and facets) in the middle of the pack as well as near the bottom (facets).  The slab on these weak layers is quite variable and hard – and though difficult to trigger, the possibility does exist. Today temperatures in the Alpine will be above freezing due to a strong inversion in our region. Ridgetops may approach 40F today. Luckily radiation from the sun is minimal at this time of year, and surface warming is expected to be subtle. Whenever temperature rise above freezing more uncertainty exists. Should the surface snow show signs of melting today it may be easier to trigger a persistent slab. This structure is most suspect on steep wind loaded slopes (Northern and Eastern) that haven’t avalanched yet. Likely trigger spots are in thinner areas near rocks. Luckily many slopes have avalanche and old debris is still very visible and is a good way to know if a slope has avalanched or not. Watch for areas with hard over soft snow and hollow sounding snow. Avoid cornices, wind pillowed snow in start zones and loaded areas farther down slope (from the strong winds). Obvious signs like cracking and ‘whumpfing’ may not be early warning signs.

Heavier loads, such as multiple snowmachines or people on the slope at one time might tip the balance. Safe travel protocol is your friend. Remember to only expose one person at a time, watch your partners, have an escape route planned, group up in safe zones and pay attention to other groups around you. 

In the periphery areas (Girdwood, Johnson/Lynx Creek and Summit Lake) where a thinner snowpack exists, several observers have experienced collapsing/whumpfing recently which indicates the potential for these persistent slab avalanches may be higher. Heighten caution is advised if traveling out of the core Turnagain Pass terrain. 

Avalanche Problem 2
  • Glide Avalanches
    Glide Avalanches
Glide Avalanches
Glide Avalanches are the release of the entire snow cover as a result of gliding over the ground. Glide avalanches can be composed of wet, moist, or almost entirely dry snow. They typically occur in very specific paths, where the slope is steep enough and the ground surface is relatively smooth. They are often proceeded by full depth cracks (glide cracks), though the time between the appearance of a crack and an avalanche can vary between seconds and months. Glide avalanches are unlikely to be triggered by a person, are nearly impossible to forecast, and thus pose a hazard that is extremely difficult to manage.
More info at Avalanche.org

Believe it or not, 3 glide avalanches have occurred last week in the Turnagain Pass zone. The first to release was on the SE aspect of Lynx Creek, followed by the SE aspect of Seattle Creek, and the SW face of Eddies. These released near the end of a 3-day inversion when temperatures in the alpine remained above freezing for multiple days. The problem with glides is that they release without warning and are not associated with human triggers. They have been known to release when temperatures are above freezing, as well as when temperatures suddenly drop. Basically glides are very unpredictable and it is best avoid being direcly below one and limit your time in run-out zones.

A glide avalanche on the SW face of Eddies released sometime between January 3rd and January 4th. Indentify existing cracks, as there are a handful that are opening up in our region. 

Weather
Sun, January 8th, 2017

Yesterday was cold and clear! Below 1000′ temperatures averaged around 0F with pockets of -10F in many valley bottoms. An inversion allowed ridgetop temps to slowly rise throughout the day from 5F to 30F by early evening. Skies were clear with light North winds. No precipitation has been recorded since December 29th.  

Clear skies and sun is expected again today along with a strong temperatures inversion that will cause valley fog in many areas of Southcentral Alaska. Temperatures could be as low as 5F near valley bottoms and approaching 40F near ridgetops. Northerly winds are forecasted to be light, 5-15mph near ridgetops.

A blocking high pressure is expected to dominate our region into the near and distant future. Expect a similar pattern over the next few days with a strong inversion, light winds, and no precipitation.

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

  Temp Avg (F) Snow (in) Water (in) Snow Depth (in)
Center Ridge (1880′) 12   0   0    34
Summit Lake (1400′) -1   0   0   11  
Alyeska Mid (1700′) 12   0   0   22  

RIDGETOP 24-hour data (6am – 6am)

  Temp Avg (F) Wind Dir Wind Avg (mph) Wind Gust (mph)
Sunburst (3812′) 29   NW   3   9  
Seattle Ridge (2400′) 24    NE 3    10
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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.

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