Turnagain Pass Avalanche Forecast RSS

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ARCHIVED FORECAST - All forecasts expire after 24 hours from the posting date/time.
Issued
Tue, March 6th, 2018 - 7:00AM
Expires
Wed, March 7th, 2018 - 7:00AM
Forecaster
Aleph Johnston-Bloom
The Bottom Line

The avalanche danger remains  MODERATE  above 1000′ on all aspects. Triggering a large slab avalanche  breaking in weak layers 1-3′ deep in the snowpack  remains possible.  Watch for old wind slabs along ridgelines and in cross-loaded gullies. Evaluate snow and terrain carefully.  

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Tue, March 6th, 2018
Alpine
Above 2,500'
Moderate (2)
Avalanche risk
Treeline
1,000'-2,500'
Moderate (2)
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
Moderate (2)
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

Observers continue to find the buried persistent weak layers in the snowpack to be reactive and the possibility of triggering a large avalanche remains.  One observer yesterday found the January 21st buried surface hoar, described the snowpack they found in Lynx Creek as “spooky” and changed their plan due to concerning snowpit test results. This buried surface hoar layer was also observed to be reactive on Magnum yesterday as well. As snow starts today and hopefully falls throughout the week it will be important to remember the current state of the snowpack. Buried 1-2′ deep are facets sitting on a crust at the mid-elevations and 1-3′ deep is a buried surface hoar/facet combo at the higher elevations. The slab over the weak layers could be very hard if it is in terrain that was affected by the strong winds last week. This was the case in the skier triggered avalanche in Summit Lake a week ago, the mid-elevation faceted layer was under very hard wind-affected snow.  Although the heart of Turnagain Pass has the buried weak layers, they are more pronounced and developed on the Southern end of Turnagain Pass and in Summit Lake where the snowpack is shallower. Areas to the North, such as Crow Pass, are also suspect along with those that have not seen much traffic this season. Using safe travel protocols and assessing the consequences if a slab does release is key in choosing terrain. Weak layers like these can become more reactive after even a small additional load. As the snow falls this week keep that in mind and as always be alert for signs of instability. 

Wind slabs: Hard wind-affected snow on steep, unsupported slopes may still triggered if you find the wrong spot. Be suspect of very stiff snow over soft snow or hollow sounding snow near upper elevation ridgelines and cross-loaded gullies. If winds really pick up this afternoon pay attention to changing conditions. 

Snowpit on Magnum yesterday at 3100′. The January 21st buried surface hoar is easy to spot and still reactive in stability tests. 

 

Cross-loaded gullies on Seattle Ridge

 

Weather
Tue, March 6th, 2018

Yesterday was mostly to partly cloudy with some afternoon sunshine peeking through. Temperatures were in the teens to mid 20Fs. Winds were light and variable. Overnight temperatures were in the teens to low 20Fs and winds remained light.  

Today will be mostly cloudy with afternoon snow showers. Temperatures will be in the teens to high 20Fs and winds will start off light and increase from the Southeast 10-20 mph gusting into the 30s. Tonight there is snow in the forecast with 2-6″ possible. Temperatures will be a bit cooler in the low 20Fs to mid teens. Winds will continue from the Southeast.  

Tomorrow’s forecast has continued snow showers in the morning, clearing in the afternoon and then more snow in the forecast overnight. The next low pressure is lining up for more snow on Thursday but details are uncertain. However, the week ahead looks to be snowy.   From the NWS discussion this morning:  Despite March and April being  the driest months of the year (climatologically), Mother Nature is  giving that statistic a run for its money. Fingers crossed!    

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

  Temp Avg (F) Snow (in) Water (in) Snow Depth (in)
Center Ridge (1880′) 22    0 0    68
Summit Lake (1400′)  12      0  0      29
Alyeska Mid (1700′)  19      0  0        59  

RIDGETOP 24-hour data (6am – 6am)

  Temp Avg (F) Wind Dir Wind Avg (mph) Wind Gust (mph)
Sunburst (3812′) 15 W    6  14
Seattle Ridge (2400′)  20 varible    3  11
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Riding Areas
Updated Wed, December 11th, 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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