Turnagain Pass Avalanche Forecast RSS

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ARCHIVED FORECAST - All forecasts expire after 24 hours from the posting date/time.
Issued
Mon, February 5th, 2018 - 7:00AM
Expires
Tue, February 6th, 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.  Additionally, watch for cornices along ridgelines and sluffs in steep terrain.  

*Periphery zones, such as 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.  

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Mon, February 5th, 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
This graphic depicts how likely you are to trigger avalanches or encounter natural avalanches while traveling on avalanche prone slopes. Unlikely means that few avalanches could be triggered in avalanche terrain and natural avalanches are not expected. The chance of triggering or observing avalanches increases as we move up the scale. Certain means that humans will be able to trigger avalanches on many slopes, and natural avalanches should be expected.

Size of Avalanches
This graphic depicts the potential size and destructive force of expected avalanches. 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, large enough to bury or destroy vehicles and break a few trees, and large enough to destroy railway cars, buildings, or a substantial amount of forest. Historic avalanches are massive events capable of destroying villages and gouging or altering the landscape.
More info at Avalanche.org

Among the thousands of snowmachine, skier and snowboard tracks around Turnagain Pass, don’t forget that a slab avalanche could still be triggered in isolated areas. These areas are more pronounced in the periphery of the forecast zone, such as South toward Johnson Pass and Summit Lake, as well as toward Portage and Girdwood Valleys. It is the higher elevation slopes that have seen prior wind loading, or have a very thin overall snowpack that are the most suspect. Keep this in mind, especially if you find yourself pushing out into terrain not yet traveled this year. 

Image on left shows Cornbiscuit near Turnagain Pass with many tracks on it without incident next to the right image of a slab triggered on Saturday in the Twin Peaks area. The Twin Peaks avalanche is on the Southern edge of the forecast zone. (Photos: left, Liz Repetto and right, Andy DuComb)

 

 

We are in a ‘normal caution’ regime at Turnagain Pass and triggering an avalanche is on the unlikely side. However, there is still snow out there that can slide, but it’s confined to isolated areas mentioned above. Below are the avalanche issues to be aware of:

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 week and a half of sunny weather. Most areas, especially in the heart of Turnagain Pass, harbor very loose snow over the buried surface hoar and only sluffs are being seen (no slab). It is the areas where the top foot or two of snow is stiffer from wind affect/loading that we need to watch out for. Also, areas where the buried surface hoar is simply deeper due to higher snowfall amounts from our last storm on January 26th, such as in the Portage Valley zone. If choosing to push into the steep and committing terrain, watch for:

–  Areas winds have affected the snow, stiffer snow over softer snow
–  Shooting cracks
–  Hand pits to see if you can find the buried surface hoar and get a block to slide off
–  Before committing to steep terrain, 
identify terrain traps like gullies, cliffs or rocks below to consider the consequences if even a small slab is released

*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 very loose and ’sluffs’ easily on the steeper slopes. Watch 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. 

Weather
Mon, February 5th, 2018

Sunny skies and light variable winds were over the region yesterday. Temperatures climbed into the mid 20’sF in the Alpine and remain there this morning. Valley bottoms warmed to the teens in many places yesterday, and have dropped back to the minus single digits this morning.

Today, skies will start clear before clouds begin to stream in mid-day, or perhaps this afternoon as a low-pressure system is headed our way for tonight/tomorrow. Ridgetop winds are expected to rise to the 5-15mph range from the East. Snowfall, up to a couple inches, is expected overnight. Temperatures will remain cold in valley bottoms today and in the 20’sF at the mid and upper elevations.

Tomorrow, Tuesday, snowfall should continue and forecast models are showing a total of 3-6″ by Tuesday evening. Temperatures will warm to around 30F at 1,000′, but should stay cold enough for snow to sea level. Ridgetop winds are expected to increase early Tuesday to the 25-30mph range from the East.

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

  Temp Avg (F) Snow (in) Water (in) Snow Depth (in)
Center Ridge (1880′) 18   0   0   62  
Summit Lake (1400′) 4   0   0   18  
Alyeska Mid (1700′) 17   0   0   50  

RIDGETOP 24-hour data (6am – 6am)

  Temp Avg (F) Wind Dir Wind Avg (mph) Wind Gust (mph)
Sunburst (3812′) 23   E   4   9  
Seattle Ridge (2400′) 24   S    4 9  
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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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