Turnagain Pass Avalanche Forecast RSS

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ARCHIVED FORECAST - All forecasts expire after 24 hours from the posting date/time.
Issued
Sat, March 7th, 2020 - 7:00AM
Expires
Sun, March 8th, 2020 - 7:00AM
Forecaster
Wendy Wagner
Avalanche risk The Bottom Line

The avalanche danger remains MODERATE. Finding and triggering a wind slab avalanche, around a foot thick, remains possible. These could be older wind slabs or new ones in areas seeing enough wind to transport snow today. They also may break wider than anticipated as some could be sitting on buried surface hoar. Additionally, there is still a chance a person could trigger a large slab avalanche that breaks in weak snow 3-6′ deep.

SUMMIT LAKE TO SEWARD REGION:  Strong wind last week impacted Summit Lake and Lost Lake, which resulted in several natural avalanches. Triggering a lingering wind slab is still possible and continued caution is advised on wind affected slopes.

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Sat, March 7th, 2020
Alpine
Above 2,500'
Moderate (2)
Avalanche risk
Treeline
1,000'-2,500'
Moderate (2)
Avalanche risk
Below Treeline
Below 1,000'
Moderate (2)
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
Moderate (2)
Danger Scale:
No Rating (0)
Low (1)
Moderate (2)
Considerable (3)
High (4)
Extreme (5)
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

Cloudy skies have moved in over the region, brought temperatures up to a more habitable 20-25°F and even a few snow flurries have fallen this morning. With a relatively weak weather system moving through this weekend, it looks as though our forecast zone will see an inch or so of snow today, 2″ tonight and up to an additional 4″ by tomorrow. This is a pretty meager ‘re-fresh’ and that said, it will be old and new wind slabs that will be our main avalanche concerns.

Lingering wind slabs from last week’s outflow wind event may still be possible to trigger. These wind slabs could propagate further than expected and could also step down into buried weak layers. This was the case with the Lynx Creek avalanche that occurred Thursday. In case you missed it, those details are HERE. These older wind slabs could be sitting on buried surface hoar, making them take longer to bond and why they could break out wider than one might think.

Fresh wind slabs are also something to look for today in upper elevation terrain. Ridgetop winds may reach averages of 20mph from the east. This will be enough to transport loose snow and load slopes, if the loose snow is available. If you are headed out today, watch for wind textured surfaces, hollow feeling snow and stiffer snow over softer snow. These are all signs of a wind slab. These slabs are likely to be around a foot thick. Quick hand pits are also good ways to suss out a wind slab. If you find one in your hand pit, look close, you may see some buried surface hoar feathers under it.

 

Wind textured surfaces along the Southeast face of Seattle Ridge at Turnagain Pass on Thursday. 3.5.20.

 

Wind loaded slopes on Colorado Peak in the Summit Lake area along with a very wide propagating natural slab avalanche lower on the slope. This also occurred also on Thursday. 3.5.20. Photo: Alex McLain

Avalanche Problem 2
  • Deep Persistent Slabs
    Deep Persistent Slabs
  • Almost Certain
    Very Likely
    Likely
    Possible
    Unlikely
    Likelihood
  • Historic
    Very Large
    Large
    Small
    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

It is still important to remember that weak faceted snow from January sits 3 to 6 feet deep in the snowpack. The wind slab triggered in Lynx Creek two days ago was a larger avalanche because it ‘stepped down’ into these old weak layers. Not only can this happen again, but it is possible a person triggers the deep layer from the start. As we know, with time the likelihood of triggering a deep slab is decreasing, but we have too much proof to write this problem off. Keeping our terrain choices in line with the ‘what if I trigger a large slab’ question remains prudent.

Cornices:  As always, avoid travel on or underneath cornices.

Loose snow avalanches:  In areas that were protected from the wind, sluffs are possible in steep terrain.

Weather
Sat, March 7th, 2020

Yesterday:  Partly cloudy to overcast skies filled the region. Ridgetop winds were light to moderate from the east (5-15mph) with Sunburst gusting to 29mph yesterday morning. Temperatures rose into the 20’s°F at most locations from sea level to ridgetops.

Today:  A weather system is moving in and brining cloudy skies and light snow showers to the forecast area. Only a trace to an inch of accumulation is expected today with 2″ of new snow possible tonight. Ridgetop winds are forecast to remain easterly and blowing in the 10-20mph range. Temperatures will remain in the 20°’F at all elevations.

Tomorrow:  Snowfall will continue tomorrow with an additional 2-4″ and up to 6″ or more in favored area likely near the coast. Ridgetop winds are slated to increase to the 15-25mph range along with the peak of snowfall looking to occur mid-day. Temperatures look to say in the mid to upper 20’s°F with snow to sea level.

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

Temp Avg (F) Snow (in) Water (in) Snow Depth (in)
Center Ridge (1880′) 21 0 0 71
Summit Lake (1400′) 18 0 0 31
Alyeska Mid (1700′) 20 trace trace 80

RIDGETOP 24-hour data (6am – 6am)

Temp Avg (F) Wind Dir Wind Avg (mph) Wind Gust (mph)
Sunburst (3812′) 13 NE 9 29
Seattle Ridge (2400′) 17 SE 7 17
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Riding Areas
Updated Thu, April 01st, 2021

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
Open
No parking in turnaround at end of the road near the outhouse.
Placer River
Open
Please do not ride along Railroad tracks. Cross tracks at 90 degree angle and clear the right of way.
Skookum Drainage
Closed
The Skookum Valley is closed to snowmachines. This closure occurs annually on April 1 as per the CNF Forest Plan.
Turnagain Pass
Open
Twentymile
Open
Please do not ride along Railroad tracks. Cross tracks at 90 degree angle and clear the right of way.
Seward District
Carter Lake
Open
Lost Lake Trail
Open
Primrose Trail
Open
Resurrection Pass Trail
Closed
Closed for the 2020/21 winter season.
Snug Harbor
Open
South Fork Snow River Corridor
Open
Summit Lake
Open

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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.

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