UPDATE: We just recieved a report of a large remote triggered avalanche in the Seattle Creek drainage that occured yesterday. We don’t have much info at this time and its unknown what layer this avalanche failed on. We do know that remote triggered avalanches are a sign of a persistent slab problem and it may be buried surface hoar. Keep this new info on your mind if you’re heading to Turnagain Pass.
Cooling temps and light winds are helping to improve stability of wind slabs since the New Year’s storm dumped 2-3’ of snow and blasted our snowpack with hurricane force winds. Clear and sunny weather today will make it easy to identify smooth pillowed convexities, cross-loaded gullies, and hollow sounding snow – wind slab habitat. What makes this avalanche problem challenging is it’s transition into becoming a persistent slab. As this storm snow problem strengthens, a layer of buried surface hoar from Christmas remains on our minds. Hand pits yesterday were challenging to find this layer due to how deeply buried (2+’) it is in places. Many observations over the last week have been documenting the location of buried surface hoar and its presence and reactivity have been variable. With that said – triggering a wind slab on a mid-storm density change or on buried surface hoar are both possible today.
If you’re headed out, ease into steeper terrain with a conservative mindset. Evaluate terrain and snow as you travel and remember ‘whumpfing’ is an obvious clue of instability.
CORNICES: There are some very large cornices along many ridgelines across our region. Triggering a cornice with the weight of a person or snowmachine is possible today. Remember these can break further back than expected. Give cornice features lots of space and avoid being directly under them.
A storm triggered slab from the New Years storm below Hippy Bowl on SW aspect of Tincan. Also note the wind sculpted snow in the alpine and cornice along the ridgeline.
Glide cracks exist in popular ski and snowmachine terrain and a may be tricky to identify with new snow covering them. Several glide cracks have avalanched this week and it’s possible more will release in the coming days. The best way to manage this problem is to avoid being under slopes with cracks opening up. They can release at any time and are not typically associated with human triggers. Glide avalanche have occurred in Lynx Creek, on Lipps, and Seattle Ridge this week.
A glide avalanche on Lipps SW face that released just before the New Years Storm is not covered by new snow and looks very different
Photo of Lipps glide crack taken yesterday (1-2-19). Although part of this crack has released the additional portion can still avalanche without warning.
South of Turnagain: A shallow and poor snowpack structure exists in the Summit Lake zone. Buried weak layers of facets associated with crusts sit near the base of the snowpack. An observation from Lynx Creek on Friday also found a reactive layer of facets mid-pack. Keep in mind Summit Lake has received additional loading from the New Years storm – strong winds and a foot of new snow. Recent avalanche activity and ‘whumpfing’ will be good reminders to keep terrain choices conservative in these zones. Triggering a larger avalanche that releases near the ground is not out of the question. Check out the Summit observations HERE for the more snowpack details.
Yesterday: Snow showers were observed in the morning with a trace of new snow at Turnagain Pass. Rain/snow line was near 300′. Light to moderate ridgetop winds from the East shifted to a NW direction by mid-day. Temperatures cooled in the upper elevations to low 20F’s/upper teens (F) as skies cleared in the afternoon.
Today: A cooling trend will continue today as a high-pressure system establishes itself over Southcentral, Alaska. Expect temps at 3000′ to reach low teens/upper single digits today. Temperatures near sea level will drop into low 20F’s to teens by this evening. Northwest ridgetop winds will be in 5-15mph range. No precipitation is expected.
Tomorrow: A similar pattern of clear skies, cold temps and light NW winds will continue into the weekend.
*Seattle Ridge weather station was heavily rimed and the anemometer (wind sensor) was destroyed.
|Temp Avg (F)||Snow (in)||Water (in)||Snow Depth (in)|
|Center Ridge (1880′)||25||trace||0||63|
|Summit Lake (1400′)||23||0||0||22|
|Alyeska Mid (1700′)||25||1||0.12||50|
|Temp Avg (F)||Wind Dir||Wind Avg (mph)||Wind Gust (mph)|
|Seattle Ridge (2400′)||21||*N/A||*N/A||*N/A|
|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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