The snowpack has shifted into a daily pattern of freezing surfaces overnight and melting surface snow in the afternoon and evening. On steep solar aspects radiation from the sun has also caused some natural wet avalanche activity later in the day. The majority of this activity has been on slopes that have rocks or dirt exposed and act as heat conductors, like Seattle Ridge which also saw a big avalanche cycle during last week’s rain event. Today we have a very warm and sunny day and calm winds today could allow surfaces to heat up more than they have in the past few days.
The best way to manage this problem is to shift over to more shaded slopes later in the day. Pay close attention to surface conditions and if you are sinking in on your skis or trenching on your snowmachine or punching through with your boots it’s a good idea to get off the slope. Push-a-lanches where the surface snow picks up momentum and entrains more surface snow is a good indicator of dangerous conditions. Avoid travel directly on or under South facing slopes later in the day. Visual clues such as recent avalanches will be tough to identify due to a widespread avalanche cycle last week. It’s really hard to tell which avalanches are new and which ones are old.
CORNICES: Cornices are very large and warm air temperatures and direct sunshine could destabilize them today. A cornice fall has the potential to trigger a very large avalanche on the slope below and could break farther back than expected. Give them a wide berth.
Seattle Ridge has been falling apart between the big wet avalanche cycle last week during a heavy rain event, natural glide avalanches, and now the sun is heating up loose snow around rocks and dirt daily.
Above 3000’ deeper snowpack instability remains a concern. A big storm event that ended on Monday and lasted two weeks dumped 5-10+ feet of snow across our region. In many places this overloaded an older snow (facets/buried surface hoar) interface and caused some very large natural avalanches. At this point there remains uncertainty if a human could trigger such a large and dangerous avalanche. Triggering this kind of avalanche would either require a very large trigger like a cornice or large wet-loose avalanche later in the day or a skier or snowmachiner finding just the right trigger spot in a shallow part of the slab. Signs of instability won’t necessarily be present and it could be the 1st or 10th skier or rider on a slope that triggers a very large destructive avalanche. All aspects and slopes above 3000’ that haven’t already avalanched are suspect. Snow pits and stability tests won’t necessarily provide representative information. This avalanche problem has become a high consequence low likelihood scenario and managing this problem is tricky. Keep in mind the following:
South of Turnagain in Summit Lake and areas in the interior Kenai Peninsula have a very poor snow structure with variety of old weak layers in the mid pack (facets and buried surface hoar.) Triggering a persistent slab 2-3’ deep as slopes warm in the afternoon sun is possible in the alpine.
A recent natural slab avalanche on a West aspect of Butch Mt in Summit Lake. The timing of this avalanche in unknown, but due to how fresh the crown appears we suspect it happened within the last two or three days. Note the older crown from last week in the lookers left corner is more filled in.
Many glide cracks have avalanched over the last few days throughout the region. The Southeast face of Seattle Ridge has seen a bunch of natural glide avalanches in the last three days. Glides are very unpredictable and fail at the ground pulling out the entire season’s snowpack. Many cracks are opening up in popular terrain and avoidance is strongly recommended. Plan your routes to avoid spending any time below existing glide cracks.
This glide crack released in the early evening yesterday also pulled out small slab with it.
Yesterday: Skies were clear and sunny. Temperatures reached the low 50Fs near sea level, upper 40Fs in the mid elevations and mid 30Fs in the upper elevations. Overnight temps at sea level and mid elevations hovered around freezing. A little cloud cover moved in overnight, but no precip was recorded. Ridgetop winds were 5-15mph from the East all day becoming light and variable overnight.
Today: Skies will be mostly sunny with some clouds in the morning. Daytime temperatures are expected to reach the mid 40Fs in the mid-elevations. In the alpine temps could reach the upper 30Fs. Ridge top winds should remain light and variable today. Overnight temperatures should drop below freezing to the upper 20Fs.
Tomorrow: High pressure and sunny skies will continue tomorrow and into next week. Similar daily temperatures are expected, mid 40Fs during the day and low 20Fs overnight. Light winds and no precipitation is expected.
|Temp Avg (F)||Snow (in)||Water (in)||Snow Depth (in)|
|Center Ridge (1880′)||38||0||0||69|
|Summit Lake (1400′)||36||0||0||22|
|Alyeska Mid (1700′)||39||0||0||63|
|Temp Avg (F)||Wind Dir||Wind Avg (mph)||Wind Gust (mph)|
|Seattle Ridge (2400′)||34||ESE||6||15|
|12/10/19||Turnagain||Avalanche: Tincan and Sunburst from the air||CNFAIC Staff|
|12/10/19||Turnagain||Observation: Tincan||Nancy Pfeiffer|
|12/08/19||Turnagain||Avalanche: Tincan||Ryan Van Luit Forecaster|
|12/06/19||Turnagain||Avalanche: Sunburst||Billy Finley|
|12/04/19||Turnagain||Observation: Sunburst||A.Johnston-Bloom/ W.Wagner/ R.Van Luit Forecaster|
|12/03/19||Turnagain||Observation: Hippy Bowl||Nick Langowski|
|12/01/19||Turnagain||Observation: Tincan, All elevations||Eric Roberts|
|12/01/19||Turnagain||Observation: Tincan||Andy Moderow|
|11/30/19||Turnagain||Observation: Tincan Treeline Plateau/ Common Bowl/ Ridge||Eric Roberts|
|11/29/19||Turnagain||Observation: Sunburst Ob #2||Aleph Johnston-Bloom Forecaster|
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: firstname.lastname@example.org
|Area||Status||Weather & Riding Conditions|
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