Turnagain Pass Avalanche Forecast RSS

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ARCHIVED FORECAST - All forecasts expire after 24 hours from the posting date/time.
Issued
Thu, January 24th, 2019 - 7:00AM
Expires
Fri, January 25th, 2019 - 7:00AM
Forecaster
Heather Thamm
The Bottom Line

The avalanche danger is HIGH above 1500′ due to strong winds and heavy snow this morning. In Girdwood and Portage Valley storm slabs 2-3+’ could release naturally. In Turnagain Pass where less snow has fallen triggering a storm slab up to 1.5′ deep is likely today on slopes greater than 30 degrees. Active wind loading, heavy precipitation and natural avalanche activity are redflag warnings to avoid avalanche terrain. The avalanche danger is CONSIDERABLE below 1500′ where wet loose snow avalanches are possible.

GIRDWOOD:  Warming temperatures and rain on old snow = ROOF AVALANCHES. Pay attention to children and pets and where you park your car.  

PORTAGE and PLACER VALLEY:    Heavier rain and snowfall rates have occurred and large avalanches above treeline may send debris to sea level and over summer hiking trails such as Byron Glacier Trail.

SUMMIT LAKE / JOHNSON PASS:    A poor snowpack structure exists in this area, which is very different than Turnagain Pass. New snow/rain and wind may overload weak layers in the snowpack and triggering a larger avalanche is possible. Look for signs of instability and pay attention to changing conditions.  

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Thu, January 24th, 2019
Alpine
Above 2,500'
High (4)
Avalanche risk
Treeline
1,000'-2,500'
High (4)
Avalanche risk
Below Treeline
Below 1,000'
Considerable (3)
Avalanche risk
Alpine
Above 2,500'
Avalanche risk
High (4)
Treeline
1,000'-2,500'
Avalanche risk
High (4)
Below Treeline
Below 1,000'
Avalanche risk
Considerable (3)
Danger Scale:
No Rating (0)
Low (1)
Moderate (2)
Considerable (3)
High (4)
Extreme (5)
Avalanche Problem 1
  • Storm Slabs
    Storm Slabs
  • Almost Certain
    Very Likely
    Likely
    Possible
    Unlikely
    Likelihood
  • Historic
    Very Large
    Large
    Small
    Size
Storm Slabs
Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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
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

Over the last two days periods of heavy snow and strong winds have created storm slabs in the mid and upper elevations of our forecast zone. The size of these slabs depends on precipitation totals and proximity to coastal areas. Portage Valley and Girdwood have received the highest amounts of precipitation and storm slabs could range from 2-3+’ in these zones. In Turnagain Pass where less snow has fallen storm slabs are expected to range from 8-16” thick. Strong Easterly ridgetop winds have been loading leeward features including a gust to 98 mph at Sunburst Wx station at 6am. Strong Easterly winds are expected to decrease to Moderate and precipitation is also expected to back off. The avalanche danger in Turnagain may decrease to CONSIDERABLE as winds decrease. If you head to an area that received less snowfall please keep in mind that triggering slab today could still be large enough to bury or kill a person. This new snow has fallen on a widespread weak layer of surface hoar  that is sitting on a hard bed surface in many places. Signs of avalanche activity, shooting cracks and collapsing are expected today and will be reminders to avoid avalanche terrain. Be aware –  another storm will impact our region overnight with up to another 1.0” of snow water equivalent (~12” of snow) expected for Turnagian and higher amounts in Girdwood and Portage.

Shooting cracks and small skier triggered storms were observed yesterday on Tincan. 

 

 

A crust bed-surface exists to 2500′ and buried surface hoar to ridgetops is also sitting under all of this new snow. This is a bad set-up for new snow to be falling on.  

Avalanche Problem 2
  • Wet Loose
    Wet Loose
  • Almost Certain
    Very Likely
    Likely
    Possible
    Unlikely
    Likelihood
  • Historic
    Very Large
    Large
    Small
    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
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

Below 2000’ where rain and wet snow have been falling the last two days natural wet loose avalanche are possible today. This avalanche hazard is most concerning in Portage Valley where a natural avalanches from above could run to valley bottoms in steep channeled terrain. Avoiding areas like Byron Glacier trail is recommended.

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

South of Turnagain – Johnson Pass/Summit Lake zone: poor snowpack structure exists in these areas.  Multiple mid-pack weak layers of facets and buried surface hoar have been found as well as a facet/crust combination in the bottom of the snowpack. Strong winds, rising temperatures and a few inches of snow over the last two days has added stress to older layers in this zone. The possibility of triggering a slab deeper in the snowpack is the primary concern in this area and a person’s weight may be enough to tip the balance. Look for signs of instability and snow and terrain carefully. 

Weather
Thu, January 24th, 2019

Yesterday: Above freezing temperatures caused precipitation to fall as rain below 1000′. A mix of rain and snow was observed below 1500′ in Turnagian Pass. Girdwood and Portage received the highest precipitation totals with Girdwood at 1.16 € SWE and Portage at 2.37 € SWE in 24 hours. Turnagain Pass DOT lot recorded 0.6 € slightly higher than the Turnagain Pass Snotel at 0.4 € SWE. Strong Easterly ridgetop winds in the yesterday morning decreased to Moderate for most of the daylight hours. Overnight Easterly ridgetop winds increased to strong averaging 30-60mph’s with a few gusts in the 90mph’s. Temperatures at sea level reached 40F’s overnight. Rain/snow line may have reached 2000′.

Today: Expect temperatures to remain around 40F at sea level and mid 30F’s at 1000′. Rain/snow line may reach 2500′. Strong winds are expected to decrease this morning to Moderate for most of the day. Tonight another storm is lined up to impact our region. Expect another round of warm temps, heavy rain and strong winds overnight.

Tomorrow: Another low-pressure system will move through our region with heavy rain expected through the morning at lower elevations. Rain/snowline is expected to be around 2500′ which means heavy snow in the upper elevations. This storm will see another round of strong Easterly winds, but winds are expected to decrease in the afternoon as the storm front passes.

 *Seattle Ridge weather station was heavily rimed and the anemometer (wind sensor) was destroyed. We are currently working to replace it.

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

  Temp Avg (F) Snow (in) Water (in) Snow Depth (in)
Center Ridge (1880′) 34   3   0.4   53
Summit Lake (1400′) 36   rain   0.1   20  
Alyeska Mid (1700′) 33   3″ wet snow   1.16   40  

RIDGETOP 24-hour data (6am – 6am)

  Temp Avg (F) Wind Dir Wind Avg (mph) Wind Gust (mph)
Sunburst (3812′) 25 ENE   33   98  
Seattle Ridge (2400′) 30   *N/A    *N/A *N/A  
Observations
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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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