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ARCHIVED FORECAST - All forecasts expire after 24 hours from the posting date/time.
Issued
Mon, December 18th, 2017 - 7:00AM
Expires
Tue, December 19th, 2017 - 7:00AM
Forecaster
Wendy Wagner
The Bottom Line

The avalanche danger is  MODERATE  on the high elevations slopes (above 3,000′) for the possibility of a slab avalanche breaking near the ground. Most concerning areas for triggering a large avalanche are where the snowpack is shallower, such as on the South side of Turnagain Pass and toward Summit Lake as well as the Crow Pass region. Additionally, a MODERATE danger exists for cornice breaks along ridgelines and lingering wind slabs at all elevations.  

*With forecasted sunny skies and fresh(ish) snow, please remember your safe travel practices! This includes, exposing one person at a time in avalanche terrain, watching your partners, being rescue ready and having an escape route planned.

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Mon, December 18th, 2017
Alpine
Above 2,500'
Moderate (2)
Avalanche risk
Treeline
1,000'-2,500'
Moderate (2)
Avalanche risk
Below Treeline
Below 1,000'
No Rating (0)
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
No Rating (0)
Danger Scale:
No Rating (0)
Low (1)
Moderate (2)
Considerable (3)
High (4)
Extreme (5)
Avalanche Problem 1
  • 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

It has been four days since the temperatures began cooling off and the extended wet storm cycles ended. It has been two days since the last snowfall. We are slowly getting a handle on the stability of the snowpack and a big thank you to all the folks that wrote in last night. We are most concerned with a known layer of faceted snow near and/or on the ground. This layer produced widespread human and natural avalanche activity during the beginning of December. The wet storms saturated the pack (and many of the facets) from 2,500′ in elevation and below, which is now locked up into stable crusts. From 2,500′ – ~3,000′ the facets remain but several thick crusts in the slab are helping to stabilize the pack. The big question is, above 3,000′ where the crusts disappear and facets under a hard slab may remain. Stability tests so far have been done up to 3,300′ and all signs point to a strong snowpack and no reactivity in the facets. See video below. This is promising. But, we must be vigilant and conservative this week as we explore the higher elevations.

Things to keep in mind:
    – 
Triggering a dangerous deep slab avalanche is possible above 3,000′
    – Shallow snowpack areas are most concerning (more trigger points and possibly more reactive facets). For instance, South end of Turnagain Pass, Crow Pass, Summit Lake
    – No red flags likely to be present to indicate an unstable pack
 

 

Pictured below is the North side of Magnum Ridge showing wind scouring and a thin snowpack. The top portion pokes into the elevation band we are concerned about. 

 

Avalanche Problem 2
  • 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 other set of avalanches problems we are still assessing are old wind slabs, cornices and sluffing. These are surface instabilities and much easier to see and assess. So far we have found good bonding with Friday’s new snow as wind slabs seem quite stubborn. However, we have only had information for a small amount of terrain. Keep an eye out for cracking in the snow around you, hollow feeling snow and stiff snow over softer snow. In most places under 2,500′ there is crust underneath, watch for area where the Friday’s snow is not bonding to this crust. 

 The SW face of Sunburst. Old avalanche debris is covered by 8″ or so of new snow from Friday, Dec 15th. 


Weather
Mon, December 18th, 2017

Partly cloudy skies were over the forecast area yesterday. During the past 48-hours there has been no precipitation. During the past 24-hours winds have been light from the East and North and temperatures in the mid 20’s at most locations. Overnight, an inversion has set in and valley bottoms are in the low teens while ridgelines are in the upper teens.

Today, we can expect a mostly sunny day. Ridgetop winds are forecast to remain light, 5-10mph from a Northerly direction and switch to Easterly tonight, remaining light. Temperatures in valley bottoms should climb during the day to the mid 20’sF while ridgetops remain in the low teens.  

Tuesday, another round of snow is headed our way as a bearing low pushes a front over Southcentral. This system looks to be cold enough for snow close to sea level, it also should favor Anchorage, Hatcher Pass and bring a several inch refresh to our neighborhood in Turnagain Pass. Make sure and check tomorrow’s advisory!

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

  Temp Avg (F) Snow (in) Water (in) Snow Depth (in)
Center Ridge (1880′) 24   0   0   33  
Summit Lake (1400′) 25   0   0   27  
Alyeska Mid (1700′)  18 0   0   10  

RIDGETOP 24-hour data (6am – 6am)

  Temp Avg (F) Wind Dir Wind Avg (mph) Wind Gust (mph)
Sunburst (3812′) *n/a   *n/a     *n/a     *n/a    
Seattle Ridge (2400′) 22   SE   4   8  
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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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