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ARCHIVED - Forecasts expire after 24 hours.
Issued
Sun, February 23rd, 2014 - 7:00AM
Expires
Mon, February 24th, 2014 - 7:00AM
Forecaster
Wendy Wagner
Avalanche risk The Bottom Line

Areas of CONSIDERABLE avalanche danger exist on recently wind loaded slopes as Easterly winds continue to transport snow at and above treeline. Natural wind slab avalanches are possible and human triggered slabs are likely on any steep slope that has seen wind loading overnight or is currently being loaded today. Slab depths could be up to 3′ thick and failing in weak snow above the January melt-freeze layer. These are unmanageable avalanche conditions with the potential for slabs to propagate wider than expected and run full path.  

On all slopes both above and below treeline without wind loading, the danger is MODERATE. In these areas, it is still possible to find and trigger a persistent slab avalanche around 2′ deep.

Special Announcements

Thanks for all the field observations from the public.  This is a huge asset to inform others of avalanche events and increases our collective knowledge of the snowpack.  Remember, you can use the  online form  or give us a voicemail using the hotline (754-2369 press star to go straight to voicemail).

Sun, February 23rd, 2014
Alpine
Above 2,500'
3 - Considerable
Avalanche risk
Treeline
1,000'-2,500'
2 - Moderate
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
  • Wind Slabs
    Wind Slabs
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.
More info at Avalanche.org

The Easterly winds that were on the rise yesterday have continued their climb overnight and are expected to level off in the ‘strong’ category today – which means averages between 26-38mph. There is plenty of loose snow available for transport and yesterday evening slopes were being rapidly loaded. At least two natural avalanches were witnessed on the SW face of Sunburst during the rapid wind loading. One was caught on video, that plus additional details HERE.

Additionally, there was one very interesting avalanche on the SW face of Sunburst that occurred earlier in the day between 12:00 and 1:00pm. It is believed to have been a natural triggered by warming plus minor wind loading. This slide occurred early enough in the day that neither the sun nor the wind was in full effect. In my mind, this shows how close to the tipping point some of these slopes are.

Below is the believed natural from around noon on the SW face of Sunburst (3,700′ elevation).  The path just to the left of this slide (partially in view) released 4 hours later, around 5:00pm and is one of the two naturals mentioned earlier.

 

For today, steering clear of steep slopes with recent wind loading will be the key to avoiding this problem. South and West aspects will be the most likely candidates for loading, but due to terrain channeling and cross-loading, all aspects are suspect including rollovers. Not only is a simple wind slab concerning enough, the fact that weak faceted snow exists under these slabs makes them downright dangerous. This is because they have the potential to be 2-3′ deep and propagate across bowls.

Avalanche Problem 2
  • 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

On slopes that are not seeing wind loading there is still the potential for triggering a persistent slab avalanche. Even though it has been over a week since Turnagain Pass has seen measurable snowfall and five days for the Girdwood Valley, we are still seeing human triggered avalanches breaking in weak snow around 2′ deep. The most recent slides were from yesterday:

1- Snowmachine triggered slab while climbing a chute in 2nd Bowl
2- Snowboarder triggered slab while descending into 1st Bowl            *Both of these are in the Seattle Creek drainage and details are limited.

On Friday, we had two large persistent slab avalanches occur. These were:

1- Skier triggered by a group ascending the headwall that joins the Magnum and Cornbiscuit ridges  – see photo below with more photos HERE plus a write up by the party HERE (Many thanks to the party for sharing their experience!).
2- Snowboarder triggered slide in Warm-up Bowl in Seattle Creek. This avalanche was reported to have a crown depth of 1-5′, width of 300′ and running to lower angle terrain.

Image is of the avalanche triggered on the headwall between Magnum and Cornbiscuit (2/21/2014, NW facing and 3,500′ elev.)

 

Although time is helping to decrease the likelihood of triggering one of these avalanches, the possibility remains. Many folks have been able to ski, snowboard and ride steep terrain without a problem – this is the hard part and why these avalanches are a roll of the dice right now. At the end of the day, it comes down to personal risk threshold. If you choose to hit the steeps, safe travel practices will help to hedge your bets. If you do not want to deal with a potentially life changing avalanche, then recreating on slopes less than 35 degrees with nothing steeper above you is the ticket. 

Sun and warming:
Due to the wind, sunshine today will likely have a hard time warming the surface snow above treeline. This includes the sun crusts on southerly aspects left over from yesterday. However, if you do find a sheltered area with enough warming, persistent slab potential will increase along with sun induced point release avalanches. Keep an eye out for any south facing start zone that is seeing intense sun, little wind and dampening surface snow.

Weather
Sun, February 23rd, 2014

Overcast skies turned mostly clear by the afternoon yesterday allowing for some welcome sunshine. What was not as welcome were the winds that gradually increased from the East / Northeast over the course of the day. Hourly averages were in the 20’s mph with gusts in the 30’s. Temperatures were on a steady rise as well with daytime highs on the ridgelines in the upper teens to 20F and the low 30’sF at 1,000. Overnight, the wind has continued its slow climb and temperature is generally holding steady.

Today will be a blustery, but clear, day in the backcountry. We are currently sitting with a dominant ridge of high pressure to our Northeast and a set of low pressure centers to our South and West. Winds should continue to  squeeze through these features from the East with ridgetop averages around 30-40mph. Temperatures are forecast to remain mild, in the mid to upper teens on ridgetops and around 30F at sea level.  

Tomorrow, Monday, this pattern persists with moderate to strong East winds, mostly clear skies and slowing warming temperatures. However, looking forward to Monday night and Tuesday a chance for a inch or two of snow is possible as a small embedded low pushes into Southcenteral. For the mid-week, models are still showing a more significant warm up.

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
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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.