Turnagain Pass RSS

Archives
ARCHIVED - Forecasts expire after 24 hours.
Issued
Tue, January 16th, 2018 - 7:00AM
Expires
Wed, January 17th, 2018 - 7:00AM
Forecaster
Aleph Johnston-Bloom
Avalanche risk The Bottom Line

The avalanche danger will rise to  HIGH  today at all elevations above 1000′ due to a storm impacting the region bringing rain, snow and strong winds. Natural and human triggered slabs 2-5+ feet deep will be likely today in avalanche terrain and may step down to older weak layers. Rain may trigger large wet loose avalanches. Travel is not recommended on slopes steeper than 30 degrees and in all runout zones.  

The avalanche danger is  CONSIDERABLE  below 1000′ where natural avalanches from above are possible in steep channeled terrain.  

Tue, January 16th, 2018
Alpine
Above 2,500'
4 - High
Avalanche risk
Treeline
1,000'-2,500'
4 - High
Avalanche risk
Below Treeline
Below 1,000'
3 - Considerable
Avalanche risk
0 - No Rating
1 - Low
2 - Moderate
3 - Considerable
4 - High
5 - Extreme
Avalanche risk Avalanche risk Avalanche risk Avalanche risk Avalanche risk
Travel Advice Generally safe avalanche conditions. Watch for unstable snow on isolated terrain features. Heightened avalanche conditions on specific terrain features. Evaluate snow and terrain carefully; identify features of concern. Dangerous avalanche conditions. Careful snowpack evaluation, cautious route-finding, and conservative decision-making essential. Very dangerous avalanche conditions. Travel in avalanche terrain not recommended. Extraordinarily dangerous avalanche conditions. Avoid all avalanche terrain.
Likelihood of Avalanches Natural and human-triggered avalanches unlikely. Natural avalanches unlikely; human-triggered avalanches possible. Natural avalanches possible; human-triggered avalanches likely. Natural avalanches likely; human-triggered avalanches very likely. Natural and human-triggered avalanches certain.
Avalanche Size and Distribution Small avalanches in isolated areas or extreme terrain. Small avalanches in specific areas; or large avalanches in isolated areas. Small avalanches in many areas; or large avalanches in specific areas; or very large avalanches in isolated areas. Large avalanches in many areas; or very large avalanches in specific areas. Very large avalanches in many areas.
Avalanche Problem 1
  • Deep Persistent Slabs
    Deep Persistent Slabs
  • Certain
    Very Likely
    Likely
    Possible
    Unlikely
    Likelihood
  • Historic (D4-5)
    Very Large (D3)
    Large (D2)
    Small (D1)
    Size
Deep Persistent Slabs
Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and 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.

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

Additional load, either from rain or snow combined with high winds, will be stressing the persistent weak layers of snow we know exist in the snowpack. We have two concerning layers of buried surface hoar and the last two days we have seen remote triggered avalanches. We have also seen avalanches stepping down and failing in weak snow near the ground. If somehow the weather doesn’t turn you away from the mountains, it is important to realize that travel in avalanche terrain is not recommended. Stay out of runout zones. Up to an inch of rain is forecasted to fall to 3000′, maybe higher. Rain to can add weight and stress the snowpack quickly. Avalanches today could be very deep and dangerous. Above 3000′ we could receive over a foot of heavy wet snow. Cornices may also release naturally and trigger slopes below.

Yesterday morning observers noticed that another portion of the Seattle Ridge avalanche path, that was observed releasing on Sunday, had also slid. The trigger is unknown. Sunday’s slide is believed to have been a remotely triggered by snowmachiners on the ridge above. This is one of the avalanches that stepped down to the ground. 

Skiers yesterday triggered a large avalanche on Eddies that connected down the ridgeline, while ski cutting a lower angle slope nearby. They reported seeing shooting cracks and then watched the slope release. The crown was 1-5′ deep (average 3′), connected approximately 600′ down the ridge and ran 700′ down the slope. No one was caught or carried. The January 11th buried surface hoar is the suspected weak layer.

Eddies avalanche, 1.15.18. Photo: Susan Goodwin

On Sunday we recieved reports of a cornice triggered slab in Main Bowl. Here is a photo of the avalanche in motion. The cornice fall is believed to have been triggered by the snowboarders on the ridge. Photo: Eric Moore

 

Avalanche Problem 2
  • Wet Loose
    Wet Loose
  • Certain
    Very Likely
    Likely
    Possible
    Unlikely
    Likelihood
  • Historic (D4-5)
    Very Large (D3)
    Large (D2)
    Small (D1)
    Size
Wet Loose
Wet Loose avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.

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

As the rain falling today saturates the surface snow to 3000′ and possibly higher expect loose wet avalanches. They are often preceded by roller balls as rain falling on dry snow can quickly break apart the bonds between snow grains. Surface snow can start failing in a point and fan out. Wet loose avalanches can gain mass as they move down hill and gather snow. They could be quite dangerous today and not something you want to mess with. These can also be triggered by skiers or riders in steep terrain. If water actually moves through the slab to the weak layers or crusts below we could get a wet slab avalanches later in day. 

 

Weather
Tue, January 16th, 2018

Yesterday skies fluctuated between broken, overcast and completely obscured. There were rain and snow showers in the afternoon, with rain falling as high at 1700′. Temperatures rose into the 30Fs. Winds were light and easterly with few gusts into the 20s.

Today is forecasted to be overcast with up to inch of rain falling to around 3000′, maybe higher. Rain could be heavy at times. Temperatures will be in the mid 30Fs at upper elevations and we could see as high 40F at 1000′. Winds will be easterly 25-35 mph gusting into the 50s. Rain fall looks to intensify tonight but rain/snow line looks to be lower, around 2400′. Temperatures overnight will be in the mid to high 30Fs and winds will be easterly, gusting into the 60s.  

Tomorrow will see a precipitation tapering off and temperatures dropping into the teens overnight. Clear, sunny weather looks to be on tap for the remainder of the week into the weekend.  

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

  Temp Avg (F) Snow (in) Water (in) Snow Depth (in)
Center Ridge (1880′) 32   0    .3 59  
Summit Lake (1400′) 28 1 .2   16  
Alyeska Mid (1700′)  34 0   .3  46

RIDGETOP 24-hour data (6am – 6am)

  Temp Avg (F) Wind Dir Wind Avg (mph) Wind Gust (mph)
Sunburst (3812′)  27  ENE 10   25  
Seattle Ridge (2400′) 30   SE   8   23  
Observations
Recent Observations for Turnagain Pass
Date Region Location
04/16/24 Turnagain Observation: Cornbiscuit
04/15/24 Turnagain Observation: Taylor Pass
04/15/24 Turnagain Observation: Seward Highway – Tern Lake to Portage
04/14/24 Turnagain Observation: Sunburst
04/14/24 Turnagain Observation: Turnagain Pass Snomo
04/13/24 Turnagain Observation: Spokane Creek
04/11/24 Turnagain Observation: Tincan
04/10/24 Turnagain Avalanche: Seattle Ridge
04/10/24 Turnagain Observation: Cornbiscuit South Face
04/10/24 Turnagain Avalanche: Tincan
Riding Areas

The riding areas page has moved. Please click here & update your bookmarks.


Subscribe to Turnagain Pass
Avalanche Forecast by Email

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.