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ARCHIVED - Forecasts expire after 24 hours.
Issued
Mon, February 12th, 2018 - 7:00AM
Expires
Tue, February 13th, 2018 - 7:00AM
Forecaster
Wendy Wagner
Avalanche risk The Bottom Line

There is a CONSIDERABLE avalanche danger above 1,000′ due to snowfall overnight and strong winds. Natural avalanches within the new storm snow are possible and human triggered avalanches are likely. Fresh wind slabs up to a foot thick, and possibly 2 feet thick, should be expected on slopes with recent wind loading. Additionally, weak layers deeper in the snowpack may become overloaded and release, creating a much larger avalanche up to 3′ thick. Below 1,000′ the danger is MODERATE for wet loose sluffs.

Special Announcements

Coming up this Friday night, Feb 16thThe 2018 SNOWBALL!! Join the  CNFAIC, our non-Profit Friends group and Alaska Avalanche School  for live music by the Hope Social Club, silent auction, raffle, locally brewed beer and good people. This benefit supports  avalanche safety in Southcentral Alaska, we look forward to seeing you there!!

Coming up Saturday, Feb 17th, from 11am-1230pmFree Avalanche Beacon Practice with CNFAIC!  We will be hosting a short workshop on how to effectively perform a companion rescuce. Open to all users and all levels; swing by on your way to the hills if your are just getting into avalanche safety or simply need a refresher!

Mon, February 12th, 2018
Alpine
Above 2,500'
3 - Considerable
Avalanche risk
Treeline
1,000'-2,500'
3 - Considerable
Avalanche risk
Below Treeline
Below 1,000'
2 - Moderate
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
  • Persistent Slabs
    Persistent Slabs
  • Certain
    Very Likely
    Likely
    Possible
    Unlikely
    Likelihood
  • Historic (D4-5)
    Very Large (D3)
    Large (D2)
    Small (D1)
    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
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

Overnight saw a quick shot of snowfall that should give us a much needed refresher. This storm was on the warm side however. Along with new moist snow that fell at the mid and upper elevations, rain has fallen up to 200-500′ in places. For storm totals at mid-elevations as of 6am this morning:

Girdwood Valley:  8-10+” snow
Turnagain Pass:  5-7″ snow
Summit Lake:  6-8″ snow

This is clearly not a large storm for our standards, but what is notable is the variety of weak layers we have within, and on the surface of, our pre-existing snowpack. Although the new snow is moist and ‘sticky’ it will likely have a hard time bonding right away onto the surface – storm snow avalanche issues are below. What is possibly more concerning is what is lurking around 1-2′ deep in our snowpack. This is a layer of buried surface hoar from Jan 21 that remains intact in many areas and could be waiting for a slab to form on top of it to start producing large avalanches. This storm has likely created that slab. Hence, today is a day to be extra cautious and evaluate the snowpack carefully. Avalanches releasing in the Jan 21 buried surface hoar could be up to 3′ thick. Also, small avalanches within the storm snow could ‘step down’ and release a much larger and unmanageable slide. This issue is less of a concern on slopes that were heavily tracked out over the past two weeks, and much more on a concern on slopes seeing moderate to no traffic. 

Photo below is from a small wind slab triggered yesterday releasing on the recently buried surface hoar. This was on the North Chutes of Cornbiscuit. Note the crack in the bed surface at the bottom of the photo. This crack is believed to have stepped down to the Jan 21 buried surface hoar, yet that layer did not slide. With more load overnight, we may see avalanche ‘step down’ to this older weak layer, creating much larger than anticipated avalanches. (Thanks to Mike Records for the photo).

Avalanche Problem 2
  • Storm Slabs
    Storm Slabs
  • Certain
    Very Likely
    Likely
    Possible
    Unlikely
    Likelihood
  • Historic (D4-5)
    Very Large (D3)
    Large (D2)
    Small (D1)
    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
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

Storm snow instabilities associated with the new snow overnight and today will be likely. These come in many forms listed below and due to the lesser snow amounts, are expected to be on the smaller side. The most concerning for us however, are wind slabs as they will likely be larger and a less manageable storm snow problem. Bonding between the new and old snow is not expected to be good as the new snow has fallen on a new crop of surface hoar and near surface facets.

Wind Slabs:  Moderate to strong winds coupled with 6-10″ of new moist snow have likely formed soft wind slabs up to a foot thick or even two feet in places. Because these slabs are likely sitting on weak old snow, they are expected to be quite sensitive and easy to trigger. 

Storm Slabs:  Out of the wind, on slopes that have more than ~5″ of new snow, expect to see soft storm slab avalanches composed of the new snow.

Loose snow sluffs:  Sluffs on steep slopes are likely with the recent new snow.

Wet sluffs:  Below 1,000′ where rain is falling on snow, small wet sluffs are likely in the steep terrain.

Roof-a-lanches:  Watch for your roofs to avalanche with the warm temperatures and rain.

Additional Concern
  • Deep Persistent Slabs
    Deep Persistent Slabs
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.
More info at Avalanche.org

Today’s snowfall is only a small load on top of our generally weak snowpack structure in the Alpine (above 3,000′). However, even a small load and warming temperatures could help tip the balance for someone to trigger a large deep slab that breaks in the bottom half of the snowpack. It’s good to remember that multiple layers of old buried surface hoar, facets and crusts exist deep in the pack and near the ground. These are not likely to ‘wake up’, but it’s worth keeping in mind, as outliers can happen as with last week’s Twin Peaks slide.

Weather
Mon, February 12th, 2018

Overcast skies were over the area yesterday along with snowfall that began late in the day, peaked overnight and is decreasing this morning. Roughly 5-10″ of new moist snow has been recorded at mid-elevations with .5-1″ of water equivalent. The rain/snow line looks to have been 200-500′. Ridgetop winds were Easterly in the 15-30mph range with gusts to 50mph. Temperatures were mild, in the mid 30’s at sea level and the mid 20’s along the ridgelines.  

Today, we should see light precipitation possibly add another 1-3″ of snow above 500′ and light rain below this in some areas. Skies will also start to clear out in certain areas as well. Ridgetop winds are expected to decrease and blow from a Southerly direction in the 5-15mph range before shifting Westerly this evening. Temperatures will remain warm, mid 30’sF at sea level and mid 20’sF along ridgetops before cooling off tonight.  

Tomorrow, Tuesday, we should see mostly clear skies, cooler temperatures and moderate to gusty Westerly winds. Another chance for snow is possible Thursday before, what looks like, mostly clear skies for late in the week.

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

  Temp Avg (F) Snow (in) Water (in) Snow Depth (in)
Center Ridge (1880′) 30   5   0.4   65  
Summit Lake (1400′) 30   5   0.5   24  
Alyeska Mid (1700′) 30   6   0.8   57  

RIDGETOP 24-hour data (6am – 6am)

  Temp Avg (F) Wind Dir Wind Avg (mph) Wind Gust (mph)
Sunburst (3812′) 21   NE   16   44  
Seattle Ridge (2400′) 24   SE   24   50  
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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.