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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
Tue, December 17th, 2019 - 7:00AM
Expires
Wed, December 18th, 2019 - 7:00AM
Forecaster
Ryan Van Luit
The Bottom Line

The avalanche danger is MODERATE in the treeline and alpine today on steep wind loaded slopes, where human triggered avalanches remain possible. Wind slabs and older storm slabs anywhere from 1 – 3′ may still be touchy after the past week of new snow and consistent winds. A chance for glide avalanches remains in the treeline band.

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Tue, December 17th, 2019
Alpine
Above 2,500'
Moderate (2)
Avalanche risk
Treeline
1,000'-2,500'
Moderate (2)
Avalanche risk
Below Treeline
Below 1,000'
No Rating (0)
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
No Rating (0)
Danger Scale:
No Rating (0)
Low (1)
Moderate (2)
Considerable (3)
High (4)
Extreme (5)
Recent Avalanches

One glide avalanche reported in the Girdwood Valley yesterday.

Avalanche Problem 1
  • Wind Slabs
    Wind Slabs
  • Almost Certain
    Very Likely
    Likely
    Possible
    Unlikely
    Likelihood
  • Historic
    Very Large
    Large
    Small
    Size
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.

Likelihood of Avalanches
Terms such as "unlikely", "likely", and "certain" are used to define the scale, with the chance of triggering or observing avalanches increasing as we move up the scale. For our purposes, "Unlikely" means that few avalanches could be triggered in avalanche terrain and natural avalanches are not expected. "Certain" means that humans will be able to trigger avalanches on many slopes, and natural avalanches are expected.

Size of Avalanches
Avalanche size is defined by the largest potential avalanche, or expected range of sizes related to the problem in question. Assigned size is a qualitative estimate based on the destructive classification system and requires specialists to estimate the harm avalanches may cause to hypothetical objects located in the avalanche track (AAA 2016, CAA 2014). Under this schema, "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. "Very Large" avalanches may bury or destroy vehicles or houses, and "Historic" avalanches are massive events capable of altering the landscape.

Signal Word Size (D scale) Simple Descriptor
Small 1 Unlikely to bury a person
Large 2 Can bury a person
Very Large 3 Can destroy a house
Historic 4 & 5 Can destroy part or all of a village
More info at Avalanche.org

Moderate winds have been consistent for the past several days, and will likely continue today at 10-20mph from the east.  These wind speeds in combination with new snow in the alpine over the past three days may create wind slabs in the lee of ridges and gullies. Pay close attention to which direction the wind is blowing, and to signs indicating which direction the wind has blown in the past.  Whumphing, cracking in the snow around you, and hollow sounds are some indicators you could be on a windslab.

Cornices continue to develop –  give them plenty of space to prevent triggering from above, and limit exposure when traveling in the runout.

Sunburst weather station data from the past week of windy weather. 

Avalanche Problem 2
  • Glide Avalanches
    Glide Avalanches
  • Almost Certain
    Very Likely
    Likely
    Possible
    Unlikely
    Likelihood
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.

Likelihood of Avalanches
Terms such as "unlikely", "likely", and "certain" are used to define the scale, with the chance of triggering or observing avalanches increasing as we move up the scale. For our purposes, "Unlikely" means that few avalanches could be triggered in avalanche terrain and natural avalanches are not expected. "Certain" means that humans will be able to trigger avalanches on many slopes, and natural avalanches are expected.
More info at Avalanche.org

Glide avalanches are unpredictable and not triggered by people. Yet there are several cracks in the Girdwood Valley and a few on Tincan in Turnagain Pass. Often, when one occurs that can be sign there could be more. There was a glide avalanche cycle in the Girdwood Valley at the end of last week and a few cracks have opened on Tincan.  If you see signs of glide cracks give them a wide berth and limit time in their runout.

Additional Concern
  • 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

In the Summit Lake area and in parts of the advisory area that have an overall shallower snowpack in the Alpine, there could be suspect layers of weak faceted snow that sit either in the mid-snowpack or base of the pack. This is above 3000′, where the snow is dryer. We have limited data from upper elevation terrain and will looking to gain more information on this.

Weather
Tue, December 17th, 2019

Yesterday:  Mostly to partly cloudy skies were over the region. Light rain in the morning and evening added between .2 – .4″ of rain below 1,500′ and 2-4″ of snow above this and into the Alpine. Ridgetop winds remained easterly and averaged in the 15-20 mph range. Temperatures have cooled slightly overnight and are sitting in the mid 30’sF at sea level and the mid 20’s F along the ridgelines.

Today:  Again partly cloudy to cloudy skies are forecast with a chance for light rain showers below 1,400′ and snow above this in some areas. Favored locations could see 2-3″ of snow by tonight at the mid and upper elevations, other areas could see clearing skies. Ridgetop winds should stay in the 10-20 mph range from an easterly direction. Temperatures look to continue on a cooling trend with the snow line creeping down to just below 1,000′ overnight where light precipitation could bring another 2″ of snow.

Tomorrow:  Intermittent snow showers (with a snow line around 1,000′) should continue through tomorrow until skies clear and we head into a cold clear period that extends through the weekend.

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

Temp Avg (F) Snow (in) Water (in) Snow Depth (in)
Center Ridge (1880′) 33 2 0.3 32
Summit Lake (1400′) 33 0 0 7
Alyeska Mid (1700′) 33 2 0.36 17

RIDGETOP 24-hour data (6am – 6am)

Temp Avg (F) Wind Dir Wind Avg (mph) Wind Gust (mph)
Sunburst (3812′) 24 NE 16 39
Seattle Ridge (2400′) N/A* N/A* N/A* N/A*

*Seattle Ridge weather station is down and as soon as the weather clears we will get it up and running!

Observations
Recent Observations for Turnagain Pass
Date Region Location
05/06/20 Turnagain Avalanche: Pastoral Peak, north face
04/10/20 Turnagain Avalanche: Wolverine
04/10/20 Turnagain Observation: Eddies lookers right shoulder
04/09/20 Turnagain Observation: Bench Peak
04/04/20 Turnagain Observation: Tincan
04/04/20 Turnagain Observation: Pete’s North
03/26/20 Turnagain Avalanche: Tincan – Proper (SW facing)
03/26/20 Turnagain Avalanche: Seattle Ridge
03/25/20 Turnagain Avalanche: Sunburst Uptrack @ 2000′
03/24/20 Turnagain Observation: Turnagain – Road Observations
Riding Areas
Updated Fri, May 01st, 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
Closed as of May 1. Thanks for a fun, safe season!
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.